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  • 1
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    GFZ Data Services
    Publication Date: 2023-01-05
    Description: Abstract
    Description: The data publication contains all heat-flow data of onshore Germany. The data release contains data generated between 1959 and 2020 and constitutes a substantial update and extension compared to the last compilation provided by the Geothermal Atlas from Hurter & Haenel (2002). The data set comprises new heat-flow determinations published after 2002 as well as data from before 2002, which were not included in the Hurter & Haenel atlas. The resulting updated database contains 836 determinations of heat flow at 595 locations from 42 publications. 85% of the reported heat-flow values are determined in boreholes, 5% in mines, and further 9 % are from onshore lake measurements using marine probe sensing techniques. The reporting and storing of the database is following the structure of the IHFC Global Heat Flow Database (Fuchs et al., 2021). A comprehensive description, including field classifications and ex-amples of associated data, is documented there. The IHFC database concept introduces parent elements (providing site-specific information), child elements (i.e. heat-flow values determined at the site and associated meta-data) and further fields providing additional information for the eval-uation of heat-flow quality. Thus, it provides a detailed collection of data and meta-data infor-mation, exceeding the sparse information on coordinates, name and heat-flow value provided in Hurter & Haenel (2002). In our release of the German heat-flow values, we have added fields about the applied quality scoring, the reasoning for inclusion or exclusion of data due to quality, and a descriptive field of the regional tectonic or geological units. For details of this procedure see Fuchs et al. (2022). The associated data description provides the full list of data sources (publications), while the DOI landing page only displays digital versions of articles if available.
    Keywords: heat flow ; geothermal potential ; onshore ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC RADIATION 〉 HEAT FLUX ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN HEAT BUDGET 〉 HEAT FLUX ; physical property 〉 temperature
    Type: Dataset , Dataset
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  • 2
    Publication Date: 2023-01-02
    Description: Abstract
    Description: This dataset includes the first order (global) distribution of frost cracking intensities (FCI) [°C m], for selected paleoclimate time-slices during Late Cenozoic, as presented in the paper by Sharma et al. (2022). The paleoclimate time-slices correspond to Pre-Industrial (~1850 CE, PI), Mid-Holocene (~6 ka, MH), Last Glacial Maximum (~21 ka, LGM) and Pliocene (~3 Ma, PLIO). The FCI (by segregation ice growth) is predicted using the approach of Andersen et al. (2015), as a function of subsurface thermal gradient and volume of (and distance to) liquid water. The paleo-temperature reconstructions are obtained from ECHAM5 general circulation model (GCM) at T159 spatial resolution (80 km * 80 km) by Mutz et al. (2018). The spatial resolution of FCI dataset is same as ECHAM5 GCM simulations (i.e. 80 km * 80 km). The dataset comprises the following: -Scripts (Python) for modeling FCI for approach described in Sharma et al. (2022). -Global FCI distribution as netCDF and ascii formats. The data is available in both netCDF and ascii formats. However, the model code (attached Python scripts) currently supports only netCDF format. The model scripts can be freely utilized for regional and local studies which require finer resolution dataset. Please refer to the associated data description file for a detailed description of the dataset.
    Description: Methods
    Description: The model is based on the approach of Andersen et al. (2015) to estimate FCI as a function of subsurface thermal gradients up to the depth of 20 m. For segregation ice growth, it additionally considers the influence of volume of water available in the proximity of an ice lens. The boundary condition includes the presence of positive temperatures (T 〉 0 °C) at either boundary (at surface or 20 m depth). The frost cracking is supported if the bedrock temperature is in the frost cracking window (–8 °C and –3 °C). The integrated FCI each grid cell, across Earth’s terrestrial surface was calculated by depth integration of the FCI averaged over a period of 1 year. The unit of FCI data is °C m.
    Keywords: Periglacial processes ; frost weathering ; frost cracking intensity ; paleoclimate ; Cenozoic ; EarthShape ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 GLACIAL PROCESSES 〉 PERIGLACIAL PROCESSES
    Type: Dataset , Dataset
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  • 3
    Publication Date: 2023-01-04
    Description: Abstract
    Description: In the near-Earth space, there are a large population of high energy electrons trapped by Earth’s magnetic field. These energetic electrons are trapped in the regions called Earth’s ring current and radiation belts. They are very dynamic and show a very strong dependence on solar wind and geomagnetic conditions. These energetic electrons can be dangerous to satellites in the near-Earth space. Therefore, it is very important to understand the mechanisms which drive the dynamics of these energetic electrons. Wave particle interaction is one of the most important mechanisms. Among the waves that can be encountered by the energetic electrons when they move around our Earth, whistler mode chorus waves can cause both acceleration and the loss of energetic electrons in the Earth's radiation belts and ring current. To quantify the effect of chorus waves on energetic electrons, we calculated the bounce-averaged quasi-linear diffusion coefficients using the chorus wave model developed by Wang et al (2019) and extended to higher latitudes according to Wang and Shprits (2019). Using these diffusion coefficients, we calculated the lifetime of the electrons with an energy range from 1 keV to 2 MeV. In each magnetic local time (MLT), we calculate the lifetime for each energy and L-shell using two different methods according to Shprits et al (2007) and Albert and Shprits (2009). We make the calculated electron lifetime database available here. Please notice that the chorus wave model by Wang et al (2019) is valid when Kp 〈= 6. If the user wants to use this lifetime database for Kp 〉6, please be careful and contact the authors.
    Keywords: Electron lifetime ; radiation belts ; ring current ; chorus waves ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 PLASMA WAVES
    Type: Model , Model
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  • 4
    Publication Date: 2023-01-09
    Description: Abstract
    Description: Mean S-wave coda quality factors (mean-Qc) were estimated from active ultrasonic transmission (UT) measurements acquired during the STIMTEC project in the URL Reiche Zeche (Saxony, Germany). We used S-coda waves of 88 selected UT measurements carried out in 3 differently oriented boreholes (BH10, BH12, BH16) to estimate the spatial change of the coda quality factor in the targeted rock volume, an anisotropic metamorphic gneiss. We also analysed temporal variation in attenuation before and after hydraulic stimulations performed in two boreholes (BH10, BH17). We formed in total 8 UT groups (see data table "2022-004_Blanke-and-Boese_mean_UT_event_locations") from neighbouring UT measurements within different depths and from separated time intervals (see also Tab. 1 in Blanke et al. 2023), and compare mean-Qc estimates of centre frequencies ranging 3-21 kHz of octave-width frequency bands. Our results show a characteristic frequency-dependence and we find that mean-Qc estimates reveal temporal-variations of attenuation more significantly than those obtained from velocity measurements. The temporal variations are strongly connected to hydraulic stimulation activities resulting in a reduction of the coda quality factor where AE events occurred. Analysis of mean-Qc estimates after a temporal resting phase (with no activity in the rock volume) suggests that frequencies 〉 15 kHz indicate healing of small-scale fractures induced by injections. The study shows that coda analysis is a powerful tool for the detection of damage zones and for monitoring changes of the local fracture network within reservoirs important for exploitation or underground storage of gases and liquids.
    Description: Methods
    Description: We applied the S-coda wave analysis of Phillips (1985), which is based on the single isotropic scattering model, to estimate the frequency dependent coda quality factor Qc for each UT measurement at each sensor in the mine. The approach of Sato (1977) allows to start the analysis early in the S-wave coda as waveforms are corrected for geometrical scattering effects. The applied method comprises two parts: 1)Moving window analysis: We followed the results of the sensitivity analysis of Blanke et al. (2019) to select the analysis parameters. We use a moving window length of 1,024 samples, a lapse time of 1.1 x ts (S-onset time), a coda length of 9,000 samples (9 ms), and a minimum signal-to-noise ratio of 2. A reference noise window is selected from the end of the seismogram. Seismograms were filtered in octave-width frequency bands and the Power Spectral Density (PSD) was estimated for the pre-defined moving windows and each frequency band. 2)Regression analysis: A regression line was fitted through the coda amplitude measurements of each frequency band. Qc values were estimated from the slopes of regression lines and uncertainties (2σ standard deviation) were calculated from the slope coefficient estimates. In a final step, mean-Qc estimates per centre frequency were estimated at each sensor for each UT group (see data tables 3-10). Mean-Qc values were estimated from a minimum of 3 neighbouring UT events. Only for group UT1BH16-AFT, some mean-Qc values were estimated from less UT events due to the short borehole section beyond a previously defined damage zone that spatially separates the UT groups.
    Description: Other
    Description: The STIMTEC hydraulic stimulation experiment (see Boese et al. 2022 for details) was conducted between 2018 and 2019 in the URL Reiche Zeche in Freiberg (Germany). The experiment aimed at investigating the role of stimulation processes in enhancing hydraulic properties of crystalline rocks. Active and passive seismic measurements were acquired in strongly foliated metamorphic gneiss during several phases of hydraulic stimulation-, testing-, and validation phases. Active measurements were conducted along two galleries (driftway and vein drift), and in several boreholes with different and mostly downward dipping orientations in the monitored rock volume (dimensions 40 m x 50 m x 30 m). The seismic network consisted of 12 Acoustic emission (AE) sensors (see data table 2), high-frequency accelerometers, and a broadband sensor installed in short and mainly upward trending boreholes above the monitored rock volume. Sensor and UT data configurations are provided by Boese et al. (2021). Hydraulic stimulations were conducted in boreholes BH10 (16-18 July, 2018) and BH17 (21-22 August, 2019) in different depth intervals and with different total injected volumes, resulting in the occurrence of AE events. This AE activity highlights activation and reactivation of fractures at the decimetre scale. The 88 analysed UT measurements (out of 〉 300) were acquired from boreholes BH10, BH12, and BH16. BH10 and BH16 run subparallel about 4.5 m apart and dip approx. 15° downwards. BH12 dips 36° from the driftway and crosses BH10 and BH16 below at approx. 33.9 and 18 m borehole depth, respectively.
    Keywords: ultrasonic transmission ; UT ; coda Q ; quality factor ; S-wave ; attenuation ; scattering ; spatio-temporal analysis ; acoustic emission ; injection ; frequency-dependency ; underground research laboratory ; URL ; Reiche Zeche ; STIMTEC ; active seismicity ; active measurements ; damage zone ; single isotropic scattering model ; borehole ; mine ; meter-scale ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES
    Type: Dataset , Dataset
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  • 5
    Publication Date: 2023-01-10
    Description: Abstract
    Description: The three datasets presented here are high-resolution catalogs containing origin time of seismic events for the same region and time range that have derived using AI-based techniques and a matched filter search. The corresponding standard catalogs from the agencies AFAD and KOERI are available under https://tdvms.afad.gov.tr/ (last accessed 28/07/2022) and http://www.koeri.boun.edu.tr/sismo/2/earthquake-catalog/ (last accessed 28/07/2022), respectively, when searching in the bulletin for longitude 28.80-29.10, latitude 40.4-40.625, and from November 1st 2018 to January 31th, 2019. Specifications for the three catalogs are. (i) Catalog derived utilizing AI-based techniques. We applied the PhaseNet deep learning method (Zhu & Beroza, 2019) to detect and pick the P-and S- waves of seismic events embedded in continuous seismic recordings from 16 stations surrounding the region of interest resampled at 100 Hz. The method was trained on a dataset from Northern California, but has been shown to generalize well to other tectonic settings. The picks were associated into seismic events using the GaMMA association method (Zhu et al., 2022). Manual check of the waveforms from all detections led to 516 seismic events with clear waveforms retained for further processing. (ii) Template matching catalog A. We applied the matched filter algorithm EQcorrscan (Chamberlain et al., 2017) to the two nearby seismic stations with the largest data recovery during the period of interest, ARMT and MDNY. We utilized 14 manually picked template events with M 〉 2 that occurred in the region of interest during the analyzed time period, which were recorded in both stations. As a first criteria to remove false detections, we retained only detections exhibiting a Median Absolute Deviation (MAD) larger than eight. We required detections from different templates to be at least 1.5 seconds apart. To remove duplicate detections (e.g., detections of the same event by different templates), we retained the detections with the highest average correlation if multiple detections occurred within 2.5 seconds. As a second criteria, we calculated cross-correlation derived phase-picks. A pick was declared if the maximum normalized correlation between the signal of the template event and of the detection exceeds 0.7. We correlated the signals in a short window of ±0.3 seconds around the assumed pick time based on a time-shifted version of the template phase-pick. We retained the S-pick exhibiting the higher cross-correlation value with respect to the template. Following this step, we considered only detections with ≥ 2 picks. In case of events with only two picks we ensured that that were from the same station to have control on the ts-tp and therefore the distance of the event from the detecting station. This catalog contains 2,462 seismic events (all manually reviewed) with magnitudes MW in the range [-2.4, 4.5]. Since we were not able to locate the events from this catalog, we considered as “origin time” the time of the first arrival. (iii) Template matching catalog B. We derived a second template matching catalog utilizing twelve of the closest seismic stations displaying high seismic data recovery during the analyzed time period. An initial list of detections was generated following the same steps as for the Template Matching Catalog A, with the additional requirement that all detections must contain at least one picks from one of the two closest stations, ARMT and MDNY. All detections from this catalog were also manually reviewed. The full description of the data processing and creation of the catalog is provided in the article “Stress changes can trigger earthquake sequences in a hydrothermal region south of Istanbul” by Martínez-Garzón et al., currently under review in Geophysical Research Letters.
    Keywords: sea level changes ; seismicity ; enhanced seismicity catalog ; Sea of Marmara region ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN WINDS ; EARTH SCIENCE 〉 OCEANS 〉 TIDES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES
    Type: Dataset , Dataset
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  • 6
    Publication Date: 2023-01-11
    Description: Abstract
    Description: South Wales is characterised by a rich variety of geologic formations and rocks of different ages and periods, and a large asymmetric syncline, as perhaps its most significant structural geological feature, extending from east to west over a length of approximately 96 km and 30 km from north to south, respectively. This oval-shaped syncline is part of the Variscan orogenic thrust and fold belt in Central Europe and covers some 2,700 km2, with coal-bearing rocks from the Upper Carboniferous (Westphalian Stage) deposited in the central syncline and older rocks outcropping in a peripheral belt around it. The coal-bearing sequence begins with Namurian grits and shales, overlain by the more productive Lower, Middle and Upper Coal Measures. A 3D structural geological model has been implemented for the central part of the South Wales Syncline and its bedrock geology. The oldest rocks in the model domain date back to the Pridoli Series from the uppermost Silurian, the youngest to the Westphalian Stage of the Upper Carboniferous. For model implementation, mainly open access data from the British Geological Survey (BGS) has been used. The final 3D structural geological model covers the entire Central South Wales Syncline and is 32.8 km wide and 36.6 km long. In total, the 3D model includes 21 fault zones and the elevation depth of ten surfaces: (1) Top Upper Coal Measures Formation; (2) Top Middle Coal Measures Formation; (3) Top Lower Coal Measures Formation; (4) Top Millstone Grit Group; (5) Top Dinantian Rocks; (6) Top Upper Devonian Rocks; (7) Top Lower Devonian Rocks (sandstone dominated); (8) Top Lower Devonian Rocks (mudstone dominated); (9) Top Pridoli Rocks; (10) Top Ludlow Rocks (in parts).
    Keywords: 3D structural geological model ; geology South Wales ; South Wales Syncline ; Central Europe ; bedrock geology ; fault zones ; geologic cross sections ; Carboniferous ; Coal Measures ; Westphalian ; Millstone Grit Group ; Dinantian Rocks ; Devonian ; Pridoli Rocks ; Silurian ; Ludlow Rocks ; Variscan Orogeny ; Variscan Foreland Basin ; coal-bearing strata ; Namurian grits ; shales ; sandstones ; siltstones ; fluvial sedimentation ; marine sedimentation ; elevation depth map ; thickness map ; LithoFrame Viewer ; Geology of Britain Viewer ; EARTH SCIENCE SERVICES 〉 MODELS 〉 GEOLOGIC/TECTONIC/PALEOCLIMATE MODELS ; Phanerozoic 〉 Mesozoic 〉 Jurassic 〉 Early/Lower Jurassic ; Phanerozoic 〉 Mesozoic 〉 Triassic ; Phanerozoic 〉 Paleozoic 〉 Carboniferous ; Phanerozoic 〉 Paleozoic 〉 Devonian 〉 Early/Lower Devonian ; Phanerozoic 〉 Paleozoic 〉 Devonian 〉 Late/Upper Devonian ; Phanerozoic 〉 Paleozoic 〉 Permian ; Phanerozoic 〉 Paleozoic 〉 Silurian 〉 Pridoli
    Type: Dataset , Dataset
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  • 7
    Publication Date: 2023-01-13
    Description: Abstract
    Description: Orbital products describe positions and velocities of satellites, be it the Global Navigation Satellite System (GNSS) satellites or Low Earth Orbiter (LEO) satellites. These orbital products can be divided into the fastest available ones, the Near Realtime Orbits (NRT, Zitat), which are mostly available within 15 to 60 minutes delay, followed by Rapid Science Orbit (RSO, Zitat) products with a latency of two days and finally the Precise Science Orbit (PSO) which, with a latency of up to a few weeks or longer in the case of reprocessing campaigns, are the most delayed. The absolute positional accuracy increases from NRT to PSO. This dataset compiles the PSO products for various LEO missions and GNSS constellation in sp3 format. GNSS Constellation: - GPS LEO Satellites: -ENVISAT -Jason-1 -Jason-2 -Jason-3 -Sentinel-3A -Sentinel-3B -Sentinel-6A -TOPEX Each solution follows specific requirements and parametrizations which are named in the respective processing metric table.
    Description: TechnicalInfo
    Description: Within the scope of various international working groups and services, and mission involvements, such as Copernicus POD QWG, IDS, ILRS, TanDEM-X, GRACE(-FO), different PSO orbits are generated at GFZ. These orbits ensue to the best of one’s ability the specific requirements and are based either on one individual observation technique or on a combination of several. Adopted processing settings and, in the case of dynamic POD, parameterizations and modeling are listed in a respective processing metric table. The orbits are stored in the GFZ Information System and Data Center (ISDC) and to the extent deemed possible freely available for the scientific community world-wide
    Keywords: Level-3 ; Satellite Geodesy ; Low Earth Orbiter ; Orbit ; TOR ; TSX ; GRACE-FO ; GPS ; RSO ; SAR ; IGOR ; Tracking ; Occultation ; Satellite Laser Ranging ; SLR ; Earth Observation Satellites 〉 ENVISAT ; Earth Observation Satellites 〉 JASON-1 ; Earth Observation Satellites 〉 OSTM/JASON-2 ; Earth Observation Satellites 〉 SATELLITES ; Earth Observation Satellites 〉 Sentinel GMES 〉 SENTINEL-3 ; Earth Observation Satellites 〉 TOPEX/POSEIDON ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 DORIS GROUND STATION BEACON ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GNSS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GPS 〉 GNSS RECEIVER ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GPS 〉 GPS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GPS 〉 GPS CLOCKS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GPS 〉 GPS RECEIVERS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GPS 〉 GPSP ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 GYROS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Laser Ranging ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Laser Ranging 〉 LASER TRACKING REFLECTOR ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Laser Ranging 〉 LRA ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Laser Ranging 〉 SLR ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Radio 〉 DORIS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Radio 〉 INS ; Earth Remote Sensing Instruments 〉 Passive Remote Sensing 〉 Positioning/Navigation 〉 Radio 〉 USO ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS ; Navigation Platforms 〉 Galileo (Europe's European Satellite Navigation System) ; Navigation Platforms 〉 GPS (Global Positioning System) ; Navigation Platforms 〉 NAVSTAR
    Type: Collection , Collection
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  • 8
    Publication Date: 2023-01-16
    Description: Abstract
    Description: This data publication contains vertical seismic profiling (VSP) data collected at the Groß Schönebeck site, Germany, from February 15-18, 2017. Energy excitation was performed with vibroseis sources. Data was acquired in the two 4.3 km deep wells E GrSk 3/90 and Gt GrSk4/05 using hybrid wireline fiber-optic sensor cables and distributed acoustic sensing (DAS) technology. The survey design and data acquisition, the overall characteristics of the acquired data, as well as the data processing and evaluation for a zero-offset source position are described in the paper of Henninges et al. (2021) published in Solid Earth. The data for several source positions presented in this paper is contained here, mostly in the form of full waveform data stored in seg-y format. A detailed description of the individual data sets is given in the attached data description document.
    Keywords: vertical seismic profiling ; fiber-optic sensing ; distributed acoustic sensing ; enhanced geothermal systems ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 ECONOMIC RESOURCES 〉 ENERGY PRODUCTION/USE 〉 GEOTHERMAL ENERGY PRODUCTION/USE ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE 〉 SEISMIC BODY WAVES ; energy 〉 energy type 〉 non-conventional energy 〉 geothermal energy ; monitoring 〉 seismic monitoring
    Type: Dataset , Dataset
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  • 9
    Publication Date: 2023-01-16
    Description: Abstract
    Description: The dataset presented in this compilation provides the input data used for the geological interpretation and for the model parameterization (Norden et al., 2022) of a 3D seismic survey in the area of the geothermal research platform Groß Schönebeck (carried out in 2017; Krawczyk et al., 2019), focussing on the deep Permo-Carboniferous geothermal targets. The geothermal research platform Groß Schönebeck is located about 50 km north of Berlin, on the southern edge of the Northeast German Basin, and is equipped with two deep wells, the E GrSk 3/90 and Gt GrSk 4/05 boreholes. In this data compilation we provide general data on the location of the boreholes and data on the applied methods and the interpretation of petrophysical properties (density, porosity, permeability, thermal properties) obtained by core analysis and well-log interpretation. Because cores were available for the E GrSk 3/90 borehole only, most of the data is referring to the borehole that was drilled more or less vertically. The other borehole (Gt GrSk 4/05) is a deviated well, drilled as a geothermal production well. Further on, we provide the main interpreted structural reflector horizons of the geological model from surface to the assumed top of sedimentary Carboniferous (for discussion of the uncertainty of this boundary please consider the comments in Norden et al., 2022) and the horizons and 3D grid properties of a parameterized simulation grid for the deep geothermal target (sedimentary Rotliegend and Permo-Carboniferous volcanic rocks).
    Keywords: Groß Schönebeck ; reservoir model ; petrophysical parameterization ; Rotliegend ; Permo-Carboniferous volcanic rocks ; EPOS ; geo-energy test beds ; compound material 〉 rock 〉 igneous rock ; compound material 〉 rock 〉 sedimentary rock ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 SEDIMENTARY ROCKS 〉 SEDIMENTARY ROCK PHYSICAL/OPTICAL PROPERTIES ; EARTH SCIENCE SERVICES 〉 MODELS 〉 GEOLOGIC/TECTONIC/PALEOCLIMATE MODELS ; In Situ/Laboratory Instruments 〉 Corers ; Models/Analyses 〉 Merged Analysis ; Phanerozoic 〉 Paleozoic 〉 Permian
    Type: Dataset , Dataset
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  • 10
    Publication Date: 2023-01-16
    Description: Abstract
    Description: An extensive vertical seismic profiling (VSP) survey using wireline distributed acoustic sensing (DAS) technology was carried out between the 15th and 18th of February 2017 at the geothermal in-situ laboratory Groß Schönebeck, Germany. Borehole measurements were recorded in two 4.3 km deep wells E GrSk 3/90 and Gt GrSk 4/05. Two hybrid fibre optics cables were freely lowered inside the wells to form dense receiver arrays. As a seismic source, four heavy vibroseis trucks were used. The survey consisted of 61 source positions distributed in a spiral pattern around the target area. This data publication consists of raw uncorrelated seismic data acquired for 3D seismic imaging purposes. Supplementary information such as well trajectories, source point coordinates, and the pilot sweep data is also provided. Data related to zero-offset measurements can be found in Henninges et al. (2021, https://doi.org/10.5880/GFZ.4.8.2021.001). Further details on the survey design and data acquisition parameters can be found in Henninges et al. (2021, https://doi.org/10.5194/se-12-521-2021); Martuganova et al. (2021, 2022). Information on high-resolution 3D reflection seismic acquisition campaign carried out at Groß Schönebeck in February–March 2017 can be found in Krawczyk et al. (2019); Bauer et al. (2020); Norden et al. (2022). The 3D DAS VSP processing workflow, 3D DAS imaging results, and comparison with 3D surface seismics are presented in Martuganova et al. (2022).
    Keywords: vertical seismic profiling ; distributed acoustic sensing ; fibre optics ; enhanced geothermal systems ; North German basin ; Groß Schönebeck ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE 〉 SEISMIC BODY WAVES
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  • 11
    Publication Date: 2023-01-18
    Description: Abstract
    Description: This publication contains software that can be used to pre-process data from the Globe at Night citizen science project, and then run an analysis to determine the rate of change in sky brightness. The software requires input data, which can be obtained directly from Globe at Night. The data used for our publication "Citizen scientists report global rapid reductions in the visibility of stars from 2011 to 2022" is published here, and can be used as input to the software. The process requires access to the World Atlas of Artificial Night Sky Brightness, which is also available from GFZ Data Services.
    Description: Other
    Description: Copyright © 2022 the authors and their institutions Licensed under the Apache License, Version 2.0 (the "License"); you may not use these files except in compliance with the License. You may obtain a copy of the License at http://www.apache.org/licenses/LICENSE-2.0. Unless required by applicable law or agreed to in writing, software distributed under the License is distributed on an "AS IS" BASIS, WITHOUT WARRANTIES OR CONDITIONS OF ANY KIND, either express or implied. See the License for the specific language governing permissions and limitations under the License.
    Keywords: light pollution ; python ; perl ; data ; naked eye limiting magnitude ; skyglow ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC RADIATION ; In Situ Land-based Platforms 〉 FIELD SURVEYS ; In Situ Land-based Platforms 〉 GROUND-BASED OBSERVATIONS ; Solar/Space Observing Instruments 〉 Photon/Optical Detectors ; The Present
    Type: Software , Software
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  • 12
    Publication Date: 2023-01-20
    Description: Abstract
    Description: The geoid for Costa Rica GCR-RSH-2020 (Geoide-Costarricense-Regional Calculado con el Método de Stokes-Helmert) is a 1 arc minute grid computed from terrestrial, marine and satellite gravity data. It is remarkable the comprehensive data cleaning and the use of new terrestrial gravity values which were not included in any other geoid determinations. The GECO global geopotential model was used for the data gap filling. The GCR-RSH-2020 computation was based on the Stokes-Helmert approach developed by the University of New Brunswick, using GOCO05s as background global geopotential model. The resulting geoid is distributed in the WGS84 system (note that between WGS84 and WRS80, there is a shift of approximately 93 cm for Costa Rica). The GCR-RSH-2020 accuracy was assessed by comparing it with GNSS/levelling values on 25 selected benchmarks of the Costa Rica vertical reference system, showing differences with a standard deviation of 0.207 m. The geoid model is provided in ISG format 2.0 (ISG Format Specifications), while the file in its original data format is available at the model ISG webpage.
    Description: Other
    Description: The International Service for the Geoid (ISG) was founded in 1992 (as International Geoid Service - IGeS) and it is now an official service of the International Association of Geodesy (IAG), under the umbrella of the International Gravity Field Service (IGFS). The main activities of ISG consist in collecting, analysing and redistributing local and regional geoid models, as well as organizing international schools on the geoid determination (Reguzzoni et al., 2021).
    Keywords: Geodesy ; Geoid model ; ISG ; UNB Stokes-Helmert approach ; Costa Rica ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS 〉 GEOID CHARACTERISTICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
    Type: Dataset , Dataset
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  • 13
    Publication Date: 2023-01-20
    Description: Abstract
    Description: Here, we present model files and example scripts for the Neural network-based model of Electron density in the Topside ionosphere (NET). The model is based on radio occultation data from Gravity Recovery And Climate Experiment (GRACE), Challenging Minisatellite Payload (CHAMP) and Constellation Observing System for Meteorology Ionosphere and Climate (COSMIC-1) missions from 2001 until 2019. The NET model is based on alpha-Chapman functions with a linear decay of scale height with altitude, and consists of 4 sub-models (2 parameters of the F2-peak and 2 parameters of the linear scale height decay). The model uses geographic and magnetic latitude and longitude, magnetic local time, day of year, altitude, solar flux index P10.7, geomagnetic activity index Kp, storm-time SYM-H index as inputs. An example data frame to run the model is provided, as well as the Jupyter notebook to perform an example run.
    Keywords: ionosphere ; machine learning ; empirical model ; neural network ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS ; EARTH SCIENCE SERVICES 〉 MODELS 〉 SOLAR-ATMOSPHERE/SPACE-WEATHER MODELS
    Type: Model , Model
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  • 14
    Publication Date: 2023-01-22
    Description: Abstract
    Description: FlotteKarte is a low-overhead plotting routine using Matplotlib, NumPy, and PyPROJ under the hood. The conceptual idea behind this package is that a map is fully defined through the 2D cartesian coordinates that result from applying the map projection to different geographical data. For displaying data on a two-dimensional canvas, Matplotlib is a powerful tool. Conversion between geographic and projected coordinates can easily be done using PyProj. The gap between these two powerful tools and a polished map lies in potential difficulties when translating spherical line topology to 2D cartesian space, and by introducing typical map decorations such as grids or ticks. FlotteKarte aims to fill this gap with a simple interface. FlotteKarte's philosophy is to work completely within the 2D projected coordinates, that is, very close to the projected data. If projected coordinates of data can be obtained, the data can be drawn directly on the underlying Matplotlib Axes. The Map class can then be used to add typical map decoration to that axes using information that it derives from the numerics of the PROJ projection.
    Keywords: cartography ; python ; EARTH SCIENCE SERVICES 〉 DATA ANALYSIS AND VISUALIZATION 〉 GEOGRAPHIC INFORMATION SYSTEMS 〉 DESKTOP GEOGRAPHIC INFORMATION SYSTEMS ; EARTH SCIENCE SERVICES 〉 DATA ANALYSIS AND VISUALIZATION 〉 STATISTICAL APPLICATIONS ; information 〉 information system 〉 geographic information system ; science 〉 geography 〉 cartography ; technology 〉 information technology 〉 multimedia technology
    Type: Software , Software
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  • 15
    Publication Date: 2023-01-24
    Description: Abstract
    Description: The Dec 22nd 2018 flank collapse and tsunami at Anak Krakatau in Indonesia is a key event in geosciences as little is known about the lead-up processes and deformation changes prior to flank failure. We processed Sentinel-1 satellite radar data in both ascending (orbit 171) and descending (orbit 47) acquisition using multi-temporal InSAR with the Small BAseline (SB) method during the 4 years prior to the collapse. The data shows that the flank was already moving for years prior to collapse, demonstrating that developing instability in volcano can be monitored long before a collapse. The southwest flank movement rates averaged approx. 27 cm/yr, but underwent intermittent accelerations coinciding with distinct intrusion events in Jan/Feb 2017 and in Jun 2018. The data archived here supplements the material detailed in Zorn et al. (202X, https://doi.org/XXXXX).
    Description: Methods
    Description: We processed the displacement flank evolution at Anak Krakatau using multi-temporal InSAR technique and exploited the Sentinel-1 data in both ascending (orbit 171) and descending (orbit 47) acquisition orbit in the period between 08th Oct 2014 and 19th Dec 2018. We adopted the Small BAseline (SB) method as implemented in the ENVI SARscape® software, using standard processing methods (Berardino et al., 2002). SB allows for a maximisation of the spatial and temporal coherence, and therefore maximises the displacement measurements over the flank, owing to the combination of interferograms with small normal and temporal baselines. We generate interferograms connecting each image with two previous and two following acquisitions. The original data has been multi-looked resulting in a pixel size of 15 m. We used the 30m resolution Shuttle Radar Topography Mission (SRTM) digital elevation model (DEM) via the Earth Resources Observation And Science (EROS) Center 2017 to remove the topographic component from the interferograms and we filter the results using Goldstein filter (Goldstein and Werner, 1998) with tile sizes of 18×18px. Finally we unwrap the interferograms masking out coherence lower than 0.2 and applying two-dimensional phase unwrapping algorithm Snaphu and we refer to the displacement measurement using a reference point located on the most northern part of the island considered stable (Fig. 2A). The final results are 1D displacement maps in ascending and descending line-of-sight (LOS). Due to a significant increase in eruptive activity of Anak Krakatau beginning towards the end of May 2018, coherence was significantly reduced on the SW-flank and many unwrapped points became unreliable and had to be filtered out. To capitalise on the previously better coverage, we split our analyses into two separate datasets, one (short) for interpreting data before the 29th May 2018, containing more reliable points on the SW-flank, and one (full) dataset with fewer points used to interpret activity after.
    Keywords: InSAR ; Volcano flank instability ; Anak Krakatau ; Collapse Hazard ; Monitoring ; Earth Observation Satellites 〉 Sentinel GMES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 TECTONIC LANDFORMS 〉 VOLCANO
    Type: Dataset , Dataset
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  • 16
    Publication Date: 2023-01-23
    Description: Abstract
    Description: The European-Mediterranean Seismological Centre (EMSC) is a non-profit scientific organization aiming at establishing and operating a rapid earthquake detection system globally and in particular in the European and Mediterranean regions as well as facilitating exchange between seismological institutes. The EMSC has been a pioneer in citizen seismology by collecting in-situ information on the earthquake impact directly from the witnesses. The EMSC has been collecting citizen intensity felt reports at a global scale for many years via two channels: its websites and its “LastQuake” smartphone application. These felt reports are collected through a set of 12 cartoons representing the 12 levels of the European Macroseismic Scale (Grünthal, 1998). They provide rapid information on how the earthquake’s impact is felt by the local population. The EMSC felt reports were shown to be consistent with the USGS Did You Feel It? (Wald et al., 2011) responses and with manually derived macroseismic datasets (Bossu et al., 2017). Such felt reports are provided for a set of 36 earthquakes, each tagged with a unique ID number. They are only considered for intensity values of up to 10, since higher values are unrealistic. Additionally, an interactive map of the aftershocks distribution is provided for each earthquake. These aftershocks are selected from the EMSC catalogue in the 14 days after the event and within 500km of the epicentre location. On each map, the beachball representing the two nodal planes as given by the Global Centroid Moment Tensor catalogue (Dziewonski et al., 1981; Ekstrom et al., 2012) is displayed at the epicentre location. For each event (identified by unique id number), the first line indicates catalogue information on the earthquake (event_id, region, origin_time (UTC), latitude, longitude, depth, magnitude, strike angle from GCMT) Each following line is a felt report gathered by the EMSC including, the longitude, latitude, reported intensity and report time.
    Keywords: felt reports ; rapid loss estimates ; crowd-sourced data ; citizen science ; finite-fault model ; EMSC ; European Mediterranean Seismological Centre ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE MAGNITUDE/INTENSITY
    Type: Dataset , Dataset
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  • 17
    Publication Date: 2023-01-23
    Description: TableOfContents
    Description: The file contains the transcriptome dataset used in the study Phylogenomics of darkling beetles (Coleoptera: Tenebrionidae) from the Atacama Desert. Directory including: Supplemental Data S1 (Data_S1). Dataset used for ML and BI analyses comprising 34 peptide precursors from 83 genera of Tenebrionidae (47 tribes, seven subfamilies), including the 30 genera from the Atacama Desert. Files: - Neuropeptide precursors matrix for ML analysis (DataS1_NP_Matrix_for_ML: amino acids in PHYLIP format). - Neuropeptide precursors matrix for BI analysis, including partitions and evolutionary models for each partition from ModelFinder (DataS1_NP_Matrix_for_BI: amino acids in NEXUS format). - Partition schemes of Neuropeptide precursors matrix for ML analysis /DataS1_ML_NP_Partition_schemes). Supplemental Data S2 (Data_S1). Dataset used for ML analysis comprising 1742 orthogroups from 83 genera of Tenebrionidae (47 tribes, seven subfamilies), including the 30 genera from the Atacama Desert. - 1742 orthogroups matrix for ML analysis (DataS2_1742_OG_ML: amino acids in PHYLIP format). - Partition schemes of 1742 orthogroups matrix for ML analysis (DataS2_1742_OG_ML_partitions_scheme)
    Keywords: Biota ; Phylogeny ; Evolution ; Insects ; Biodiversity
    Type: Dataset , Dataset
    Format: ZIP
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  • 18
    Publication Date: 2023-01-23
    Description: Abstract
    Description: The European-Mediterranean Seismological Centre (EMSC) is a non-profit scientific organization aiming at establishing and operating a rapid earthquake detection system globally and in particular in the European and Mediterranean regions as well as facilitating exchange between seismological institutes. The EMSC has been a pioneer in citizen seismology by collecting in-situ information on the earthquake impact directly from the witnesses. The EMSC has been collecting citizen intensity felt reports at a global scale for many years via two channels: its websites and its “LastQuake” smartphone application. These felt reports are collected through a set of 12 cartoons representing the 12 levels of the European Macroseismic Scale (Grünthal, 1998). They provide rapid information on how the earthquake’s impact is felt by the local population. The EMSC felt reports were shown to be consistent with the USGS Did You Feel It? (Wald et al., 2011) responses and with manually derived macroseismic datasets (Bossu et al., 2016). This dataset includes four ".csv" files in total. The file, "felt_reports_2014_2021.csv" and "catalog_2014_2021.csv" contain an exhaustive set of globally collected felt reports between January 2014 and December 2021, and the corresponding earthquake catalog, respectively. The files "felt_reports_2022.csv" and "catalog_2022.csv" contain felt reports for a selection of 11 well reported earthquakes from 2022 and the corresponding earthquake catalog, respectively. This data is the foundation of the work by Lilienkamp et al. (2023).
    Keywords: Citizen Science ; Macroseismic observations ; Rapid Disaster Response ; EARTH SCIENCE SERVICES 〉 HAZARDS MANAGEMENT 〉 DISASTER RESPONSE ; technology 〉 information technology 〉 multimedia technology ; The Present
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  • 19
    Publication Date: 2023-02-08
    Description: Abstract
    Description: The Institute of Seismology, University of Helsinki (ISUH) was founded in 1961 as a response to the growing public concern for environmental hazards caused by nuclear weapon testing. Since then ISUH has been responsible for seismic monitoring in Finland. The current mandate covers government regulator duties in seismic hazard mitigation and nuclear test ban treaty verification, observatory activities and operation of the Finnish National Seismic Network (FNSN) as well as research and teaching of seismology at the University of Helsinki.The first seismograph station of Finland was installed at the premises of the Department of Physics, University of Helsinki in 1924. However, the mechanical Mainka seismographs had low magnification and thus the recordings were of little practical value for the study of local seismicity. The first short-period seismographs were set up between 1956 and 1963. The next significant upgrade of FNSN occurred during the late 1970’s when digital tripartite arrays in southern and central Finland became fully operational, allowing for systematic use of instrumental detection, location and magnitude determination methods. By the end of the 1990’s, the entire network was operating using digital telemetric or dial-up methods. The FNSN has expanded significantly during the 21st Century. It comprises now 36 permanent stations. Most of the stations have Streckeisen STS-2, Nanometrics Trillium (Compact/P/PA/QA) or Guralp CMG-3T broad band sensors. Some Teledyne-Geotech S13/GS13 short period sensors are also in use. Data acquisition systems are a combination of Earth Data PS6-24 digitizers and PC with Seiscomp/Seedlink software or Nanometrics Centaurs. The stations are connected to the ISUH with Seedlink via Internet and provide continuous waveform data at 40 Hz (array) or 100-250 Hz sampling frequency. Further information about instrumentation can be found at the Institute’s web site (www.seismo.helsinki.fi). Waveform data are available from the GEOFON data centre, under network code HE, and arefully open.
    Keywords: geophysics ; seismology ; seismic noise ; earthquakes ; induced ; seismic hazard ; broad band ; velocity ; acceleration ; displacement ; Monitoring system ; Seismological stations ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
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  • 20
    Publication Date: 2023-02-08
    Description: Abstract
    Description: – A temporary seismic network consisting of 48 long-term and 15 short-term stations was deployed from June 2021 to June 2022. The network comprises 27 broadband stations and 20 short period geophones from the Ruhr-University Bochum, the Geophysical Instrument Pool Potsdam (GIPP) and the RWTH Aachen. The inter-station spacing of the longer-term network is about 2 km and the total extent of the network is about 20 km. The densely populated area and vicinity of active pit mining demanded a balance between dense station placement and avoidance of anthropogenic noise sources. The network serves as a pre-study for the installment of a field laboratory in Eschweiler-Weisweiler, Germany. Details can be found in the accompanying data publication (Finger et al., in preparation). This project has been subsidized through the Cofund GEOTHERMICA, which is supported by the European Union’s HORIZON 2020 programme for research, technological development and demonstration under grant agreement No 731117. Furthermore, this study was supported by the Interreg North-West Europe (Interreg NWE) Programme through the Roll-out of Deep Geothermal Energy in North-West Europe (DGE-ROLLOUT) Project (http://www.nweurope.eu/DGE-Rollout), NWE 892. The Interreg NWE Programme is part of the European Cohesion Policy and is financed by the European Regional Development Fund (ERDF). Waveform data are available from the GEOFON data centre, under network code ZB. Data from some stations are embargoed until Januar 2026 but might be available on request.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; temporary local seismic network ; passive seismology ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~1T
    Format: .mseed
    Format: XML
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  • 21
    Publication Date: 2023-02-08
    Description: Abstract
    Description: Volcanic eruptions are regularly observed on the island of Fogo, Cape Verde, with an average re-occurrence interval of ca. 20 years. However, the structure and extent of the related volcanic plumbing system are not well understood. Previous studies have investigated earthquakes related to magmatic processes connected with the Fogo volcano using conventional network configurations. Seismicity has been reported to occur mainly southwest of the island of Brava while a more recent study reports on activity focussed between Brava and Fogo. Multi-array seismology has the potential to significantly reduce the localization errors of seismic events in particular for those outside a station network and to lower the detection threshold. The subject of this study is the investigation of the local volcano-related seismicity applying multi-array methods which is a unique task amongst the research activities at German universities. The scientific aims are (a) to precisely map local events to constrain the structure of and the dynamic processes within the volcanic plumbing system, (b) to image the magma source region below the Fogo volcano using reflected and backscattered waves, and (c) to localize low-frequency volcanic tremor events. Waveform data are available from the GEOFON data centre, under network code 9J, and are embargoed until February 2022.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; temporary local seismic network ; Monitoring system ; Seismological stations ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~1T
    Format: .mseed
    Format: XML
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  • 22
    Publication Date: 2023-02-08
    Description: Abstract
    Description: This data publication is supplementary to the study on headwall erosion rates at Glacier d'Otemma in Switzerland, by Wetterauer et al. (2022). Debris on glacier surfaces stems from steep bedrock hillslopes that tower above the ice, so-called headwalls. Recently, rock walls in high-alpine glacial environments experience increased destabilization due to climate warming. Since supraglacial debris alters the melt behaviour of the ice underneath, increased headwall erosion and debris delivery to glacier surfaces will modify glacial mass balances. Therefore, we expect that the response of glaciers to climate change is likely linked to how headwall erosion responds to climate change. As headwall debris is deposited on the ice surface of valley glaciers it is passively transported downglacier, both supra- and englacially. Where two glaciers join, debris along their margins is merged to form medial moraines. Since medial moraine debris tends to be older downglacier, systematic downglacier-sampling of medial moraine debris and the measurement of in situ-produced cosmogenic 10Be concentrations ([10Be]) hold the potential to assess long-term (〉10^2-10^4 yrs) headwall erosion rates through time. However, to obtain the cosmogenic signals of headwall erosion, [10Be] within supraglacial debris need to be corrected for glacial transport time, as cosmogenic nuclides continue to accumulate during exposure and transport. This additional 10Be accumulation during debris transport can be accounted for by simple downglacier debris trajectory modelling. Providing our 10Be dataset together with detailed information on our 1-D modelling approach is the main objective of this data publication. The data is presented as one single xlsx-file with three different tables. A detailed description of the sample processing and the debris trajectory model are provided in the data description file of this data publication. For more information see our study Wetterauer et al. (2022).
    Description: Other
    Description: The data were collected as part of the project “COLD”, which investigates the Climate Sensitivity of Glacial Landscape Dynamics with a focus on the European Alps. This research receives funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program under grant agreement 759639.
    Keywords: Alpine glaciers ; medial moraines ; cosmogenic 10Be ; grain size ; headwall erosion rates ; supraglacial debris ; EARTH SCIENCE 〉 LAND SURFACE 〉 EROSION/SEDIMENTATION 〉 EROSION ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 GLACIAL LANDFORMS 〉 MORAINES 〉 MEDIAL MORAINE
    Type: Dataset , Dataset
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  • 23
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. One sample of thermal water was taken from the production well at Balmatt, Belgium on May 17th 2021 and sent to Hydroisotop for analysis of main cations and anions and heavy metals. It can be seen that the nitrate content is remarkably high. However, all meaurements had to be conducted from the same sample bottle, which had been acidified, presumably with HNO3 which can be expected to be the source of the high nitrate content. The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Antimony (mg/l),Barium (mg/l),Iodide (mg/l),Lithium (mg/l),Silicon (mg/l),Strontium (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Iron total (mg/l),Copper (mg/l),Manganese total (mg/l),Nickel (mg/l),Uranium (mg/l),Zinc (mg/l) Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C).
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626/de
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 24
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. At Neustadt-Glewe one thermal water sample was taken by GFZ on June 02, 2021 and sent to Hydroisotop for analysis of main cations, anions, heavy metals, DOC, gases and isotopes (18O, 2H, 18O-SO4, 2H, 13C-DIC, 13C-CO2, 13C-CH4, 13C-CxHy, 2H-CH4, 34S-SO4, 34S-H2S, 2H-CH4). There was too little H2S in sample 363469 to conduct the 34S-H2S measurement. The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Spec. electr. conductivity (25 degC) Lab.,pH value Lab.,Temperature Lab. (degC),Alkalinity (pH 4.3) Lab. (mmol/l),Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Ammonium (mg/l),Hydrogen carbonate (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Antimony (mg/l),Barium (mg/l),Fluoride (mg/l),Iodide (mg/l),Lithium (mg/l),Silicon (mg/l),Strontium (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Chromium total (mg/l),Iron total (mg/l),Copper (mg/l),Manganese total (mg/l),Nickel (mg/l),Uranium (mg/l),Zinc (mg/l),DOC (mg/l),Hydrogen (Nml/kg),Oxygen (Nml/kg),Nitrogen (Nml/kg),Carbon dioxide (Nml/kg),Methane (Nml/kg),Ethane (Nml/kg),Propane (Nml/kg),Butane (Nml/kg),Pentane (Nml/kg),Helium (Nml/kg),Argon (Nml/kg),Sum Gases (Nml/kg),Oxygen-18 d18O-H2O (per mille VSMOW),Deuterium d2H-H2O (per mille VSMOW),Deuterium-excess (per mille VSMOW),Carbon-13 d13C-DIC (per mille VPDB),Sulphur-34 d34S-SO4 (per mille V-CDT),Oxygen-18 d18O-SO4 (per mille VSMOW),Carbon-13 d13C-CO2 (per mille VPDB),Carbon-13 d13C-CH4 (per mille VPDB),Deuterium d2H-CH4 (per mille VSMPW),Carbon-13 d13C-C2H6 (per mille VPDB),Carbon-13 d13C-C3H8 (per mille VPDB),Carbon-13 d13C-i-C4H10 (per mille VPDB),Carbon-13 d13C-n-C4H10 (per mille VPDB) Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C) .
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 EARTH GASES/LIQUIDS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 25
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. In order to gain information about the increased methane content (about 65 vol-%) in the gas samples of the Groß Schönebeck production well (GrSk05/05) collected in February 2021 as compared to previous samples in 2010-2018 (10-14 vol-%), three gas samples were sampled by GFZ on 02 March 2021 at the valve at the wellhead when releasing the pressure from the wellhead. Main gas composition was measured by GFZ indicating again predominantly CH4 (63,9-64,2 Vol-%) followed by N2 (30,9 – 31,2 vol.-%) with minor amounts of H2 (3,4 vol-%) and CO2 (0,01-0,04 vol-%). Potential reasons for the increased methane content could be either microbial activity or contribution of fluid / gas from a different source within the reservoir. To determine the origin of methane, therefore, isotope analyses were performed. The samples arrived at Hydroisotop on March 13th 2021 for the analysis of higher hydrocarbons (C2-C5) and their isotopic composition (13C-CO2, 13C -CH4, 13C-CxHy and 2H-CH4). Together with the measured high amounts of higher hydrocarbons (ethane, propane etc.) they indicate a rather thermogenic source of the hydrocarbons. To better clarify the question of the source of methane, additionally, two downhole water samples from two different depths (1500 and 4000 m) were taken by GFZ on 09th and 10th of June 2021 and sent to Hydroisotop for analysis of main cations and anions, heavy metals, trace elements and isotopes (13C-CH4) in July 2021. The water sample composition resembles those of earlier measurements of samples collected in Groß Schönebeck (e.g. Regenspurg et al., 2010). However, since the well had not been in operation for a while a depth differentiation between the sample from 4000 m and the one from 1500 m is obvious. This was already visible by the black precipitate observed in the 4000 m sample, whereas the sample at 1500 m showed da reddish precipitate of presumably iron oxides. It should be noted that the nitrate content of the water samples is unusually high since reducing conditions are expected. This could have been caused by air contact of the sample and subsequent oxidation. Furthermore, a reduced silicon content shows in sample 365871 compared to sample 365870. Given the high temperature of the well, the higher silicon content is more plausible. The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Antimony (mg/l),Barium (mg/l),Bromide (mg/l),Fluoride (mg/l),Iodide (mg/l),Lithium (mg/l),Silicon (mg/l),Strontium (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Copper (mg/l),Manganese total (mg/l),Nickel (mg/l),Uranium (mg/l),Zinc (mg/l),Ethane (vpm),Propane (vpm),i-Butane (vpm),n-Butane (vpm),i-Pentane (vpm),n-Pentane (vpm),Ethene (vpm),Propene (vpm),1-Butene (vpm),Carbon-13 d13C-CO2 (per mille VPDB),Carbon-13 d13C-CH4 (per mille VPDB),Deuterium d2H-CH4 (per mille VPDB),Carbon-13 d13C-C2H6 (per mille VPDB),Carbon-13 d13C-C3H8 (per mille VPDB),Carbon-13 d13C-i-C4H10 (per mille VPDB),Carbon-13 d13C-n-C4H10 (per mille VPDB) Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C).
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 EARTH GASES/LIQUIDS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 26
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. On 10th of May 2021, two thermal water samples were taken by TNO before and after the heat exchanger at the geothermal site Heemskerk in the Netherlands. The samples sent to Hydroisotop were analysed for their hydrochemical composition, heavy metal and dissolved organic carbon (DOC) content and stable isotopes (18O, 2H, 13C-DIC). It should be noted that the pH measured in the laboratory diverges from previously observed pH values which in the past have not been reported below 5,4. Concentrations of major ions had initially been reported too low but re-measurement of the samples yielded values in ranges that had previously been recorded. However, the concentraton of Lithium is much higher than expected. In order to resolve these uncertainties, the site Heemskerk will be sampled again. The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Spec. electr. conductivity (25 degC) Lab. (muS/cm),pH value Lab.,Temperature Lab. (degC),Alkalinity (pH 4.3) Lab. (mmol/l),Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Ammonium (mg/l),Hydrogen carbonate (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Antimony (mg/l),Barium (mg/l),Fluoride (mg/l),Iodide (mg/l),Lithium (mg/l),Silicon (mg/l),Strontium (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Iron total (mg/l),Copper (mg/l),Manganese total (mg/l),Nickel (mg/l),Uranium (mg/l),Zinc (mg/l),DOC (mg/l),Oxygen-18 d18O-H2O (per mille VSMOW),Deuterium d2H-H2O (per mille VSMOW),Deuterium-excess (per mille VSMOW),Carbon-13 d13C-DIC (per mille VPDB). Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C)
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 27
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. On 29th and 30th of April 2021 five thermal water samples were taken by Hydroisotop from five different springs/wells located at Wildbad-Einöd. The samples were analysed for hydrochemical composition, heavy metals and dissolved organic carbon (DOC) content. It can be noted that the bromide content of sample 361625 is much lower than the bromide content in the other four springs. Since the chloride content in all springs is the same order of magnitude and Cl/Br ratios are expected to be similar in the same The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Temperature at sampling (degC),Spec. electr. conductivity (25 degC) at sampling (muS/cm),Spec. electr. conductivity (25 degC) Lab. (muS/cm),pH value at sampling,pH value Lab.,Temperature Lab. (degC),Dissolved oxygen content (mg/l),Redox potential (mV),Base capacity (pH 8.2) (mmol/l),Alkalinity (pH 4.3) on site (mmol/l),Alkalinity (pH 4.3) Lab. (mmol/l),Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Ammonium (mg/l),Hydrogen carbonate (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Nitrite (mg/l),Bromide (mg/l),Fluoride (mg/l),Iodide (mg/l),Lithium (mg/l),Silicon (mg/l),Strontium (mg/l),Iron total (mg/l),Manganese total (mg/l),DOC (mg/l) Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C)
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 28
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. At the geothermal site Blumau in Austria five thermal water samples were taken by Hydroisotop at the production and injection well, as well as after the heat exchanger on 29th of June 2020. Besides the hydrochemical composition, dissolved gases, the heavy metal content, DOC and stable isotopes (18O, 2H, 13C-DIC) were analysed. Additionally, three thermal water samples were taken by the operator on 09th of March 2021 and sent to Hydroisotop for DOC measurements. The dataset contains analysis results associated with the research project reflect. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory,Lab No.,Sampling date,Temperature at sampling (degC),Spec. electr. conductivity (25 degC) at sampling,Spec. electr. conductivity (25 degC) Lab. (muS/cm),pH value at sampling,pH value Lab.,Temperature Lab. (degC),Dissolved oxygen content (mg/l),Redox potential (mV),Alkalinity (pH 4.3) Lab. (mmol/l),Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Ammonium (mg/l),Hydrogen carbonate (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Nitrite (mg/l),Antimony (mg/l),Barium (mg/l),Boron (mg/l),Bromide (mg/l),Fluoride (mg/l),Iodide (mg/l),Molybdenum (mg/l),Ortho-phosphate (mg/l),Selenium (mg/l),Strontium (mg/l),Sulphide total (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Cadmium (mg/l),Chromium total (mg/l),Cobalt (mg/l),Iron total (mg/l),Copper (mg/l),Nickel (mg/l),Mercury (mg/l),Zinc (mg/l),Tin (mg/l),DOC (mg/l),Hydrogen (Nml/kg),Oxygen (Nml/kg),Nitrogen (Nml/kg),Carbon dioxide (Nml/kg),Methane (Nml/kg),Ethane (Nml/kg),Propane (Nml/kg),Butane (Nml/kg),Pentane (Nml/kg),Ethene (Nml/kg),Propene (Nml/kg),Helium (Nml/kg),Argon (Nml/kg),Sum Gases (Nml/kg),Oxygen-18 d18O-H2O (per mille VSMOW),Deuterium d2H-H2O (per mille VSMOW),Deuterium-excess (per mille VSMOW),Carbon-13 d13C-DIC (per mille VPDB) Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C).
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 EARTH GASES/LIQUIDS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 29
    Publication Date: 2023-02-09
    Description: Abstract
    Description: The main objective of the work package 2 of the REFLECT project is to characterise relevant fluid properties and their reactions for saline fluids (type C). One of the specific goals was to collect fluid samples from several saline fluids from geothermal sites across Europe, determine their properties, and thus contribute to the Fluid Atlas (WP3). Additionally, the REFLECT team will compare those field data with data from lab experiments performed at near natural conditions. Samples of type C fluids were taken from several sites in Germany, Austria, Belgium and the Netherlands. The samples were analysed for major and minor ions, dissolved gases and isotopes. Two thermal water samples were taken by Hydroisotop at the production and injection wells in Insheim on 18th of June 2020. The samples were analysed for their hydrochemical composition, heavy metal and dissolved organic carbon (DOC) content, dissolved gases and stable isotopes of water and gas components (18O, 2H, 34S-H2S, 34S-SO4, 18O-SO4, 13C-DIC, 13C-CO2, 13C-CH4, 2H-CH4). Nitrate and a positive redox potential is present in both water samples when reducing conditions would be expected in a deep geothermal well. On-site measurements showed no oxygen present. It is however possible that air contamination during sampling caused some ammonium to oxidize to nitrate. The dataset contains analysis results associated with the research project REFLECT. It is a comma separated file (csv) containing the following columns: Location,Country,Description,Laboratory (Lab.),Lab. No.,Sampling date,Temperature at sampling (degC),Spec. electr. conductivity (25 degC) at sampling (muS/cm),Spec. electr. conductivity (25 degC) Lab. (muS/cm),pH value at sampling,pH value Lab.,Dissolved oxygen content (mg/l),Redox potential (mV),Base capacity (pH 8.2) (mmol/l),Alkalinity (pH 4.3) on site (mmol/l),Alkalinity (pH 4.3) Lab. (mmol/l),Sodium (mg/l),Potassium (mg/l),Calcium (mg/l),Magnesium (mg/l),Ammonium (mg/l),Hydrogen carbonate (mg/l),Chloride (mg/l),Sulphate (mg/l),Nitrate (mg/l),Antimony (mg/l),Barium (mg/l),Bromide (mg/l),Fluoride (mg/l),Iodide (mg/l),Lithium (mg/l),Molybdenum (mg/l),Total phosphate (mg/l),Ortho-phosphate (mg/l),Silicon (mg/l),Strontium (mg/l),Sulphide total (mg/l),Aluminium (mg/l),Arsenic (mg/l),Lead (mg/l),Iron total (mg/l),Copper (mg/l),Manganese total (mg/l),Nickel (mg/l),Uranium (mg/l),Zinc (mg/l),DOC (mg/l),Hydrogen (Nml/kg),Oxygen (Nml/kg),Nitrogen (Nml/kg),Carbon dioxide (Nml/kg),Methane (Nml/kg),Ethane (Nml/kg),Propane (Nml/kg),Butane (Nml/kg),Pentane (Nml/kg),Helium (Nml/kg),Argon (Nml/kg),Sum Gases (Nml/kg),Oxygen-18 d18O-H2O (per mille VSMOW),Deuterium d2H-H2O (per mille VSMOW),Deuterium-excess (per mille VSMOW),Carbon-13 d13C-DIC (per mille VPDB),Sulphur-34 d34S-SO4 (per mille V-CDT),Sulphur-34 d34S-H2S (per mille V-CDT),Oxygen-18 d18O-SO4 (per mille VSMOW),Carbon-13 d13C-CO2 (per mille VPDB),Carbon-13 d13C-CH4 (per mille VPDB),Deuterium d2H-CH4 (per mille VPDB). Methods are described in the accompanying deliverable Fluid data of geothermal sites (type C)
    Description: Other
    Description: Project summary: The efficiency of geothermal utilisation largely depends on the behaviour of fluids that transfer heat between the geosphere and the engineered components of a power plant. The Horizon 2020 funded project REFLECT aims to avoid problems related to fluid chemistry rather than treat them. Fluid physical and chemical properties are often poorly defined, as in situ sampling and measurements at extreme conditions have proved difficult to date. Therefore, large uncertainties in current model predictions prevail, which are being tackled in REFLECT by collecting new, high-quality data in critical areas. The data is being implemented in a European geothermal fluid atlas and in predictive models to allow recommendations on how to best operate geothermal sites sustainably and to enhance geothermal technology development. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement nº 850626. Project website: https://www.reflect-h2020.eu/ Cordis website: https://cordis.europa.eu/project/id/850626/de
    Keywords: geothermal ; hydrothermal ; REFLECT ; Redefining geothermal fluid properties at extreme conditions to optimize future geothermal energy extraction ; EARTH SCIENCE 〉 SOLID EARTH 〉 EARTH GASES/LIQUIDS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 GROUNDWATER CHEMISTRY
    Type: Dataset , Dataset
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  • 30
    Publication Date: 2023-02-09
    Description: Abstract
    Description: In September 2017 three crustal-scale seismic profiles were acquired in southern Iran covering the subaerial accretionary wedge of the western part of the Makran Subduction zone. Each of the roughly north-south trending profiles was approximately 200 km long, and on each profile 9 to 10 artificial shots with charges between 400 and 800 kg of explosives were fired. The seismic signals were observed by 300 autonomous digital recorders with geophones on each profile. This dataset consists of the raw (continuous) data of the recorders (in proprietary cube format and MSEED-format) and the shot records in SEGY-format (standard exchange formats).
    Description: Other
    Description: The Geophysical Instrument Pool Potsdam (GIPP) provides field instruments for (temporary) seismological studies (both controlled source and earthquake seismology) and for magnetotelluric (electromagnetic) experiments. The GIPP is operated by the GFZ German Research Centre for Geosciences. The instrument facility is open for academic use. Instrument applications are evaluated and ranked by an external steering board. See Haberland and Ritter (2016) and https://www.gfz-potsdam.de/gipp for more information.
    Keywords: subduction zone ; accretionary wedge ; Makran ; deep seismic sounding ; crustal structure ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WIDE-ANGLE_REFLECTION_REFRACTION ; CONTROLLED_SOURCE_SEISMOLOGY 〉 EXPLOSION_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 WEIGHT-DROP_SOURCE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 CRUSTAL_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 REGIONAL_SCALE ; CONTROLLED_SOURCE_SEISMOLOGY 〉 DSS ; SENSOR 〉 GEOPHONE ; SENSOR 〉 VERTICAL_COMPONENT ; LAND ; SEG-Y_DATA_FORMAT ; MINISEED_DATA_FORMAT ; SEISMIC_WAVEFORM_DATA ; CONTROLLED_SOURCE_SEISMOLOGY 〉 RAW_DATA ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE ; In Situ/Laboratory Instruments 〉 Profilers/Sounders 〉 SEISMIC REFLECTION PROFILERS
    Type: Dataset , Dataset
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  • 31
    Publication Date: 2023-02-09
    Description: Abstract
    Description: 24 European annually resolved stable isotope chronologies have been constructed from tree ring cellulose for the last 400 years (1600CE – 2003CE) for carbon and oxygen and for the last 100 years for hydrogen. Data was produced within the ISONET project (400 Years of Annual Reconstructions of European Climate Variability Using a Highly Resolved Isotopic Network,) to initiate an extensive spatiotemporal tree-ring stable isotope network across Europe funded as part of the fifth EC Framework Programme “Energy, Environment and Sustainable Development”. This data set comprises the ISONET δ18O records.
    Description: Methods
    Description: Wood increment cores of 15 or more Pinus sylvestris, Quercus robur/petraea or Cedrus atlantica tree individuals were taken. Dendro-dated tree-ring material of 4-5 individuals per site was dissected and pooled year by year. After cellulose extraction and homogenization, 18O/16O-ratios of annually resolved samples were determined by Isotope Ratio Mass Spectrometry (IRMS). Time series of 18O/16O are given as d-values versus SMOW. Details can be found in the downloadable “data description” file.
    Description: Other
    Description: The ISONET project has been striving to improve greatly our understanding of European climate systems providing independent quantitative data for model verification and policy making. A network of 24 sites provides dendrochronological coverage from Iberia to Fennoscandia, Caledonia and the Tyrol. The stable isotope (C, H, O) ratios of these annually resolved time series shall be analysed within this project, to reconstruct past climate regimes (temperature, relative humidity and precipitation characteristics) for the last 400 years. Climate variability shall be addressed on three timescales; decade-century (source water/air mass dominance); inter-annual (quantifying baseline variability, extreme events and recent trends); and intra-annual (high resolution exploration of seasonality signals within tree-rings). ISONET goes far beyond existing tree-ring analyses in its spatial based investigation and interpretation (see also https://cordis.europa.eu/project/id/EVK2-CT-2002-00147).
    Type: Dataset , Dataset
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  • 32
    Publication Date: 2023-02-10
    Description: Other
    Description: The ISONET project has been striving to improve greatly our understanding of European climate systems providing independent quantitative data for model verification and policy making. A network of 24 sites provides dendrochronological coverage from Iberia to Fennoscandia, Caledonia and the Tyrol. The stable isotope (C, H, O) ratios of these annually resolved time series shall be analysed within this project, to reconstruct past climate regimes (temperature, relative humidity and precipitation characteristics) for the last 400 years. Climate variability shall be addressed on three timescales; decade-century (source water/air mass dominance); inter-annual (quantifying baseline variability, extreme events and recent trends); and intra-annual (high resolution exploration of seasonality signals within tree-rings). ISONET goes far beyond existing tree-ring analyses in its spatial based investigation and interpretation (see also https://cordis.europa.eu/project/id/EVK2-CT-2002-00147).
    Description: Abstract
    Description: 24 European annually resolved stable isotope chronologies have been constructed from tree ring cellulose for the last 400 years (1600CE – 2003CE) for carbon and oxygen and for the last 100 years for hydrogen. Data was produced within the ISONET project (400 Years of Annual Reconstructions of European Climate Variability Using a Highly Resolved Isotopic Network,) to initiate an extensive spatiotemporal tree-ring stable isotope network across Europe funded as part of the fifth EC Framework Programme “Energy, Environment and Sustainable Development”. This data set comprises the ISONET δ13C records.
    Description: Methods
    Description: Wood increment cores of 15 or more Pinus sylvestris, Quercus robur/petraea or Cedrus atlantica tree individuals were taken. Dendro-dated tree-ring material of 4-5 individuals per site was dissected and pooled year by year. After cellulose extraction and homogenization, 18O/16O-ratios of annually resolved samples were determined by Isotope Ratio Mass Spectrometry (IRMS). Time series of 13C/12C are given as d-values versus PDB. Details can be found in the downloadable “data description” file.
    Type: Dataset , Dataset
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  • 33
    Publication Date: 2023-02-14
    Description: Abstract
    Description: The data set comprises petrophysical laboratory data for four carbonate rocks and one sandstone – both in solid rock and crushed state. Rock plugs and particle packings of intentionally crushed and sieved material are investigated. Thereby, eight particle size classes with a mean diameter between 0.032 and 9.66 mm are investigated. The data set includes complex electrical conductivity (from Spectral Induced Polarization – SIP), specific surface (from nitrogen adsorption) and porosity (from mercury intrusion MIP). Further analyses include e.g. particle geometry, Nuclear Magnetic Resonance (NMR), Scanning Electron Microscopy (SEM), Computer Tomography (μCT), uniaxial compression strength and mineralogical composition (chemical analysis, XRD).
    Keywords: petrophysics ; laboratory ; crushed rock ; cuttings ; inversion ; particle ; carbonate ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS ; EARTH SCIENCE SERVICES 〉 MODELS 〉 PHYSICAL/LABORATORY MODELS ; physical property 〉 electricity ; science 〉 natural science 〉 earth science 〉 geophysics
    Type: Dataset , Dataset
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  • 34
    Publication Date: 2023-02-14
    Description: Abstract
    Description: A low blank, high-precision, and highly reproducible technique for Boron (B) isotope analysis performed by Multi-Collector-Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS), Thermo Scientific Neptune PlusTM was developed and is presented here. We show data on a set of international certified standard materials (NIST SRM 951) and various kind of matrices (B1-IAEA, B2-IAEA, B3-IAEA, B4-IAEA, B5-IAEA, and JB-2) measured with MC-ICP-MS Neptune Plus, focusing on the accuracy and reproducibility of the analyses performed in the Neptune-TIMS Laboratory
    Keywords: Boron Isotopes ; MC-ICP-MS ; Neptune ; EPOS ; multi-scale laboratories ; geochemistry and microscopy ; geochemistry data ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 MC-ICP-MS
    Type: Dataset , Dataset
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  • 35
    Publication Date: 2023-02-14
    Description: Abstract
    Description: Results of a high throughput, robust and sensitive method for the precise analysis of 87Sr/86Sr by Multi-Collector-Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS), Thermo Scientific Neptune PlusTM are reported. The data were obtained after accurate procedures of chemical separation and purification of Sr from geological matrices such as silicates, sulfides, carbonates and waters, using Eichrom Sr-spec resins as well as the routine for Sr isotope measurement. Mass discrimination and instrument drift were corrected by using natural constant 86Sr/88Sr ratios as an internal standard. Data on set of international certified standard materials (SRM NIST 987 and AGV-1) as well as intra-lab reference samples (water sample KGV-9) measured with MC-ICP-MS Neptune Plus, focusing on the accuracy and reproducibility of the analyses performed in the Neptune-TIMS Laboratory are here reported.
    Keywords: Strontium Isotope ; MC-ICP-MS ; Neptune ; Isotope Ratios ; EPOS ; multi-scale laboratories ; geochemistry and microscopy ; geochemistry data ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 MC-ICP-MS
    Type: Dataset , Dataset
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  • 36
    Publication Date: 2023-02-14
    Description: Abstract
    Description: We describe here in detail the results and the setup of the high precision Nd isotope ratio analysis performed by Multi Collector Inductively Coupled Plasma Mass Spectrometer (MC ICP MS), Thermo Scientific Neptune Plus TM. Isobaric interferences and mass discrimination were corrected by using natural invariable 147Sm/144Sm and 146Nd/144Nd isotope ratios. We reported data on set of international certified standard materials (JNdi-1 and AGV-1) measured with MC-ICP-MS Neptune Plus, focusing on the accuracy and reproducibility of the analyses performed in the Neptune-TIMS Laboratory
    Keywords: Neodymium Isotope ; MC-ICP-MS ; Neptune ; EPOS ; multi-scale laboratories ; geochemistry and microscopy ; geochemistry data ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 MC-ICP-MS
    Type: Dataset , Dataset
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  • 37
    Publication Date: 2023-02-14
    Description: Abstract
    Description: We describe here in detail the results and the setup of the high precision Pb isotope ratio analysis performed by Multi Collector Inductively Coupled Plasma Mass Spectrometer (MC ICP MS), Thermo Scientific Neptune Plus TM. We performed this method adding thallium (Tl) as an internal isotopic standard to correct mass dependent isotopic fractionation. We also report the procedures for the chemical separat ion and purification of Pb from geological matri ces such as silicates , sulfides and historical artefacts . We report the data obtained on the international certified standard material SRM NIST 981 measured with MC ICP MS Neptune Plus, focusing on the accuracy and reproducibility of the analyses performed in the Neptune TIMS Laboratory (IGG-CNR in Pisa, Italy), and highlighting the advantages brought by the installation of this new mass spectrometer.
    Keywords: Lead Isotopes ; MC-ICP-MS ; Neptune-TIMS Laboratory ; Isotope Ratios ; EPOS ; multi-scale laboratories ; geochemistry and microscopy ; geochemistry data ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 MC-ICP-MS
    Type: Dataset , Dataset
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  • 38
    Publication Date: 2023-02-14
    Description: Abstract
    Description: This data publication contains the compilation of global heat-flow data by the International Heat Flow Commission (IHFC; http://www.ihfc-iugg.org/) of the International Association of Seismology and Physics of the Earth's Interior (IASPEI). The presented data release 2021 contains data generated between 1939 and 2021 and constitutes an updated and extended version of the 2012 IHFC database release (IHFC 2012; later re-published as PANGAEA release: Global Heat Flow Compilation Group, 2013). The 2021 release contains 74,548 heat-flow data from 1,403 publications. 55% of the reported heat-flow values are from the continental domain (n ~ 40,870), while the remaining 45% are located in the oceanic domain (n ~ 33,678). The data are provided in csv and Excel formats. Compared to earlier compilations, which followed the structure defined by Jessop et al. (1976), the new data release was transformed to the recently redefined structure for reporting and storing heat-flow data in the Global Heat Flow Database (Fuchs et al., 2021). Therefore, the notation and structure of the database was adopted, transforming the database field entries defined after Jessop et al. (1976) to the new field structure. Old code notations are not continued and the dataset was cleaned for entries without reporting any heat-flow value. Although successfully transformed, this release marks an intermediate step as the majority of the newly defined database fields have not been filled yet. Filling these fields, checking the existing entries and assessing the quality of each entry are the aim of the upcoming Global Heat Flow Data Assessment Project, for which this data set provides the basis. Consequently, we kindly ask the user to take notice that the current release still suffers similar problems as previously published compilations in terms of data heterogeneity, documentation and quality.
    Keywords: International Heat Flow Database ; IASPEI ; heat flow ; EARTH SCIENCE 〉 LAND SURFACE 〉 SOILS 〉 THERMAL CONDUCTIVITY ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN HEAT BUDGET ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN HEAT BUDGET 〉 CONDUCTION ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL TEMPERATURE
    Type: Dataset , Dataset
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  • 39
    Publication Date: 2023-02-14
    Description: Abstract
    Description: The data publication contains the compilation of global heat-flow data by the International Heat Flow Commission (IHFC; www.ihfc-iugg.org) of the International Association of Seismology and Physics of the Earth's Interior (IASPEI). The presented data update 2023 contains data generated between 1939 and 2022 and constitutes the first intermediate update benefiting from the global collaborative assessment and quality control of the Global Heat Flow Database running since May 2021 (http://assessment.ihfc-iugg.org).
    Keywords: heat flow density ; Global Heat Flow Database ; International Heat Flow Commission ; EARTH SCIENCE 〉 OCEANS 〉 MARINE VOLCANISM 〉 BENTHIC HEAT FLOW ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN HEAT BUDGET 〉 HEAT FLUX ; physical property 〉 temperature
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  • 40
    Publication Date: 2023-02-15
    Description: Abstract
    Description: The data publication contains all heat-flow data of offshore in the Guaymas basin. The data release contains data generated between 1959 and 2019 and constitutes a substantial update and extension compared to the last compilation provided by Becker & Fisher (1991). The data set comprises new heat-flow determinations published after 1991 as well as data from before 1991, which were not included in the Becker & Fisher (1991). The resulting updated database contains 487 determinations of heat-flow at 464 locations from 17 publications. 95% of the reported heat-flow values are determined from marine probe sensing technique and 5% in boreholes.
    Description: Methods
    Description: The reporting and storing of the database are following the structure of the IHFC Global Heat Flow Database (Fuchs et al., 2021). A comprehensive description, including field classifications and examples of associated data, is documented there. The IHFC database concept introduces parent elements (providing site-specific information), child elements (i.e., heat-flow values determined at the site and associated meta-data) and further fields providing additional information for the evaluation of heat flow quality. Thus, it provides a detailed collection of data and meta-data information, exceeding the sparse information on coordinates, name and heat-flow value.
    Keywords: Heat flow ; Guaymas Basin ; IODP ; EARTH SCIENCE 〉 OCEANS 〉 MARINE VOLCANISM 〉 BENTHIC HEAT FLOW ; physical property 〉 temperature
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  • 41
    Publication Date: 2023-02-18
    Description: Abstract
    Description: This dataset provides friction and elasticity data from ring shear and axial tests, respectively, on rock analogue materials used at the University Roma Tre (Rome, IT) in “Foamquake”, a novel seismotectonic analog model mimicking the megathrust seismic cycle (Mastella et al., under review). Two granular materials (quartz sand and Jasmine rice) have been characterized by means of internal friction coefficients µ and cohesions C. An elastic material (foam rubber) have been characterized by means of Young’s modulus E and Poisson’s ratio v. According to our analysis the granular materials show Mohr-Coulomb behaviour characterized by linear failure envelopes in the shear stress vs. normal load Mohr space. Peak, dynamic and reactivation friction coefficients of the quartz sand are µP = 0.69, µD = 0.56 and µR = 0.64, respectively. Cohesion ranges between 50 and 100 Pa. Rate-dependency of friction in quartz sand seems insignificant. Peak, dynamic and reactivation friction coefficients of the Jasmine rice are µP = 0.70, µD = 0.59 and µR = 0.61, respectively. Cohesion ranges between 30 and 50 Pa. Rate-weakening of Jasmine rice is c. 6% per tenfold change in shear velocity v. The Young’s modulus of the foam rubber has been constrained to 30 kPa, its Poisson’s ratio is v=0.1.
    Keywords: multiscale laboratories ; analogue models of geologic processes ; property data of analogue modelling materials ; analogue ; EPOS ; Cohesion ; Density ; Digital Image Correlation (DIC) / Particle Image Velocimetry (PIV) 〉 StrainMaster (La Vision GmbH) ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 PLATE BOUNDARIES ; Earthquake simulator ; Flour 〉 Rice ; Foam rubber ; Force sensor ; Friction coefficient ; geolocical hydrogeological 〉 earthquake ; megathrust ; Poisson ratio ; Python ; Ring-shear tester ; Sand 〉 Quartz Sand ; Subduction box ; tectonic and structural features ; tectonic process 〉 subduction ; tectonic setting 〉 plate margin setting 〉 forearc setting ; tectonic setting 〉 plate margin setting 〉 subduction zone setting ; Time lapse camera ; Triaxal tester ; Uniaxial tester ; Young modulus
    Type: Dataset , Dataset
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  • 42
    Publication Date: 2023-02-23
    Description: Abstract
    Description: In coastal Arctic permafrost regions, thermokarst lagoons represent the transition state from a freshwater lacustrine to a marine environment, and receive little attention regarding their role for greenhouse gas production and release. The geochemical features of a thermokarst lagoon were compared with two thermokarst lakes on the Bykovsky Peninsula in northeastern Siberia. This data set includes pH, major cations and anions, alkalinity, salinity, and dissolved iron (ferric and ferrous) concentrations from porewater of lake and lagoon sediments; the concentration and stable isotopic signature of CH4 in small plug samples from the sediment cores; total carbon (TC), total organic carbon (TOC), total nitrogen (TN), and total sulfur (TS) measured from the bulk sediment; and several biomarker indices (e.g. CPI, Paq) were calculated based on n-alkane concentrations to characterize the origin of organic matter (OM) in the lakes.
    Keywords: thermokarst lake ; themokast lagoon ; carbon turnover ; geochemistry ; EARTH SCIENCE 〉 LAND SURFACE 〉 FROZEN GROUND 〉 PERMAFROST
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  • 43
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    GFZ Data Services
    Publication Date: 2023-02-24
    Description: Abstract
    Description: The classical way to model the stress state in a rock volume is to estimate displacement boundary conditions that minimize the deviation of the modelled stress state with respect to model-independent stress information such as stress magnitude data. However, these data records are usually subject to significant uncertainties and measurement errors. Hence, it has to be expected that not all stress magnitude data records are representative and can be used in a model. In order to identify unreliable stress data records, the stress state that is based on individual data records is solved and compared with observations at a few discrete locations. While this method works, it is not efficient in that most of the solved model scenarios will be discarded. The solving of the entire model consumes immense amount of computation time for a high-resolution model. Yet, the stress state is required at only a very limited number of locations. For linear geomechanical models it is sufficient to estimate the stress state from three model scenarios with arbitrary, but different displacement boundary conditions. These three results can be used to estimate analytically using a linear regression at discrete points stress states based on user-defined boundary conditions. The tool Fast Automatic Stress Tensor Estimation (FAST Estimation) is a Python function that automatizes this approach. FAST Estimation provides very efficiently the stress states at pre-defined locations for all possible boundary conditions. It does not provide the continuous stress field as provided by a solved geomechanical model. Instead, it is a cost-efficient solution for the rapid assessment of stress states at a limited number of discrete locations based on pre-defined boundary conditions.
    Description: Other
    Description: Copyright © 2023 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany FAST Estimation is free software: you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation, either version 3 of the License, or (at your option) any later version. FAST Estimation is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License for more details. You should have received a copy of the GNU General Public License along with this program. If not, see http://www.gnu.org/licenses/.
    Keywords: geomechanical-numerical model ; stress ; in-situ stress ; model calibration ; stress tensor calibration ; modelling tool ; model quality assessment ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 NEOTECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 CRUSTAL MOTION 〉 CRUSTAL MOTION DIRECTION ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 FAULT MOVEMENT ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 PLATE BOUNDARIES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 STRESS
    Type: Software , Software
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  • 44
    Publication Date: 2023-03-01
    Description: Abstract
    Description: This data publication represents the main outcomes of WP1.200 of Individual Project IP1 and Deliverable D1.1 of the research unit NEROGRAV. The goal of WP1.200 was the realistic representation of modern ocean tide model uncertainties in the form of empirical Variance-Covariance Matrices (VCMs) for the utilization in satellite gravimetric dealiasing. In the following, we describe the data set generation and format. A more detailed description of the processing strategy of the data set can be found in Abrykosov et al. (2021).
    Description: Other
    Description: A deep understanding of mass distribution and mass transport in System Earth is needed to answer central questions in hydrology, oceanography, glaciology, geophysics and climate research. The necessary information is primarily derived from satellite mission data as observed by GRACE (Gravity Recovery and Climate Experiment) and GRACE-FO (Follow-on) describing the gravity field of the Earth and its temporal variations. The research group (RG) „New Refined Observations of Climate Change from Spaceborne Gravity Missions (NEROGRAV)”, funded by the German Research Foundation (DFG), develops since May 2019 new analysis methods and modeling approaches to improve GRACE and GRACE-FO mission data analysis and focuses on geophysical applications that benefit from significantly reduced error levels in the time series of monthly gravity fields. Phase 1 lasted from May 2019 till April 2022. After successful evaluation in January 2022 the second phase started in January 2023. The central hypothesis of the research group, slightly updated for phase 2, is: Only by concurrently improving and better understanding of sensor data, background models, and processing strategies of satellite gravimetry, the resolution, accuracy, and long-term consistency of mass transport series can be significantly increased; the science return in various fields of application improved and the potential of future technological sensor developments fully exploited. All groups participating in NEROGRAV have a long-term heritage of expertise in geodetic data acquisition and modeling and will additionally contribute their unique complementary expertise from various neighboring disciplines such as oceanography, hydrology, solid Earth, geophysics and atmospheric and climate sciences. Therefore, it is expected that the second funding phase will not only create significantly improved GRACE/GRACE-FO gravity field models over two decades, but also enable geophysical applications based on this long-term series such as quantifying North Atlantic deep water transports as indicator for variations in the Atlantic Meridional Overturning Circulation (AMOC), assessment of hydrometeorological extreme events or identification of climatic signatures in variations of the terrestrial water storage. Important results and datasets of phase 1 can be found at GFZ Data Services.
    Keywords: satellite gravimetry ; Stokes coefficients ; Covariance ; empirical VCM ; NEROGRAV ; New Refined Observations of Climate Change from Spaceborne Gravity Missions ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE ; EARTH SCIENCE 〉 OCEANS 〉 MARINE GEOPHYSICS 〉 MARINE GRAVITY FIELD ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN WAVES 〉 GRAVITY WAVES ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL COMPONENTS ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL HEIGHT
    Type: Dataset , Dataset
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  • 45
    Publication Date: 2023-03-01
    Description: Abstract
    Description: This data publication represents the main outcomes of WP4.100 of Individual Project IP4 and of the Deliverable D4.1 of the research unit NEROGRAV summarizing the analyses of the GRACE and GRACE-FO accelerometer (ACC) and satellite-to-satellite tracking data (Microwave instrument (MWI) or Laser Ranging Interferometer (LRI)) in order to derive a characterization of the instrument performance and a stochastic model. A detailed description and discussion focusing on the GRACE data is given in Murböck et al. (submitted to Remote Sensing). This first version of the combined ACC+MWI/LRI noise models is provided with the ASCII-file NEROGRAV_Dataset_GRACE_GRACE-FO_ACC-MWI-LRI_StochasticModel_V01.dat containing header information (17 lines) and the square root power spectral densities (PSDs), i.e. the amplitude spectral densities (ASDs) for the combined accelerometer and ranging observations in terms of range-rates (cf. Fig. 1). It is given for 21600 frequencies from 1/86400 Hz up to 0.25 Hz. Above 0.1 Hz (Nyquist frequency of the 5 s sampled MWI data) the columns for the ACC+MWI models are zero. The five columns consist of the frequency in Hz (col. 1), the combined ACC+MWI models for GRACE 2007 (col. 2), GRACE 2014 (col. 3), GRACE-FO 2019 (col. 4) and the combined GRACE-FO 2019 ACC+LRI model (col. 5) in m/s/√Hz.
    Type: Dataset , Dataset
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  • 46
    Publication Date: 2023-03-01
    Description: Abstract
    Description: The dataset (Mielke et al, 2023) consists of daily ASCII-files, each containing the spherical harmonic coefficients (SHCs) for atmosphere, hydrology, and ocean bottom pressure. The files that include the AH+O coefficients are provided in the AOD format of the GFZ with the naming convention TYPE_YYYY-MM-DD_X_01.asc and contain header information (30 lines) and four columns with degree (n) order (m) and Stokes coefficients cnm and snm. Coefficients in each file are split up into different subsets, each corresponding to a subdaily time step (i.e., a daily file with 3-hour temporal resolution is split up into 8 subsets). The entire dataset is organized following the folder structure /TYPE/NEST/coeff_aodFormat_XXX/. We provide regional refined (nested), coarse grained (nested, but with a lower resolution version of the regional model), or global model solutions of SHCs for each datatype. Some datasets are available in different spectral resolutions, with d/o up to 179, 180, or 360. In this release all AH+O coefficients have a temporal resolution of 3 hours, except the non-regional refined atmospheric solution, which is given 6-hourly. Currently, the whole data set is provided for June 2007 and some components for the whole year 2007. Additional months and years will be added with newer versions of the dataset or can be provided by the authors on request. For the atmospheric and hydrological background model, regional models with high spatial and temporal resolution are nested into global models: Therefore, global and regional models must be resampled and interpolated on the same regular grid with equivalent time epochs. For the nesting, the global model is interpolated on the same grid resolution as the regional model. Grid points of the global model are than replaced with the data of the regional model of the CORDEX-EU region. A Gaussian filter is applied in a transition zone with a width of 7.5° to reduce an edge effect (Gibbs effect) between the two combined models.
    Description: Other
    Description: A deep understanding of mass distribution and mass transport in System Earth is needed to answer central questions in hydrology, oceanography, glaciology, geophysics and climate research. The necessary information is primarily derived from satellite mission data as observed by GRACE (Gravity Recovery and Climate Experiment) and GRACE-FO (Follow-on) describing the gravity field of the Earth and its temporal variations. The research group (RG) „New Refined Observations of Climate Change from Spaceborne Gravity Missions (NEROGRAV)”, funded by the German Research Foundation (DFG), develops since May 2019 new analysis methods and modeling approaches to improve GRACE and GRACE-FO mission data analysis and focuses on geophysical applications that benefit from significantly reduced error levels in the time series of monthly gravity fields. Phase 1 lasted from May 2019 till April 2022. After successful evaluation in January 2022 the second phase started in January 2023. The central hypothesis of the research group, slightly updated for phase 2, is: Only by concurrently improving and better understanding of sensor data, background models, and processing strategies of satellite gravimetry, the resolution, accuracy, and long-term consistency of mass transport series can be significantly increased; the science return in various fields of application improved and the potential of future technological sensor developments fully exploited. All groups participating in NEROGRAV have a long-term heritage of expertise in geodetic data acquisition and modeling and will additionally contribute their unique complementary expertise from various neighboring disciplines such as oceanography, hydrology, solid Earth, geophysics and atmospheric and climate sciences. Therefore, it is expected that the second funding phase will not only create significantly improved GRACE/GRACE-FO gravity field models over two decades, but also enable geophysical applications based on this long-term series such as quantifying North Atlantic deep water transports as indicator for variations in the Atlantic Meridional Overturning Circulation (AMOC), assessment of hydrometeorological extreme events or identification of climatic signatures in variations of the terrestrial water storage. Important results and datasets of phase 1 can be found at GFZ Data Services.
    Keywords: New Refined Observations of Climate Change from Spaceborne Gravity Missions ; NEROGRAV ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE ; EARTH SCIENCE SERVICES 〉 MODELS 〉 ATMOSPHERIC GENERAL CIRCULATION MODELS ; EARTH SCIENCE SERVICES 〉 MODELS 〉 HYDROLOGIC AND TERRESTRIAL WATER CYCLE MODELS ; EARTH SCIENCE SERVICES 〉 MODELS 〉 OCEAN GENERAL CIRCULATION MODELS (OGCM)/REGIONAL OCEAN MODELS
    Type: Dataset , Dataset
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  • 47
    Publication Date: 2023-03-02
    Description: Abstract
    Description: High resolution debris thickness mapping using land surface temperature maps (LST) and surface energy balance modelling (SEBM). LST data was produced by a radiometric thermal infrared measurements from an uncrewed aerial vehicle (UAV). The SEBM considers the rate of change of heat storage as an energy balance component derived from diurnal temperature variablity.
    Description: Other
    Description: Licence: Licence: GNU General Public Licence (Version 3, 19 November 2007) Copyright (C) 2022 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences (Deniz Gök) This program is free software: you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation, either version 3 of the License, or (at your option) any later version. This program is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License for more details. You should have received a copy of the GNU General Public License along with this program. If not, see http://www.gnu.org/licenses/〉.
    Keywords: debris-covered glaciers ; debris thickness ; surface energy balance model ; Aircraft 〉 UAV ; EARTH SCIENCE 〉 LAND SURFACE 〉 LAND TEMPERATURE 〉 LAND SURFACE TEMPERATURE
    Type: Software , Software
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  • 48
    Publication Date: 2023-03-04
    Description: Abstract
    Description: GRACE monthly gravity field solutions starting from April 2002 to June 2017 up to degree and order 90 computed with the Celestial Mechanics Approach at AIUB. The time series is an updated of AIUB-RL02 GRACE monthly gravity field time series using Level-1B GRACE data and updated background models. The dataset is created within the framework of the G3P - Global Gravity-based Groundwater Product project (https://www.g3p.eu/), this project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 870353.
    Description: Other
    Description: Parameters: product_type = gravity_field earth_gravity_constant = 3.986004415000e+14 radius = 6.378137000000e+06 max_degree = 90 norm = fully_normalized tide_system = tide_free errors = formal
    Keywords: International Center for Global Earth Models ; ICGEM ; Gravity Recovery And Climate Experiment ; GRACE ; GRACE-FO ; Level-2 ; SHM ; Spherical Harmonic Model ; Gravitational Field ; Geopotential ; Gravity Field ; Time variable Gravity Field ; Satellite Geodesy ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
    Type: Dataset , Dataset
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  • 49
    Publication Date: 2023-03-03
    Description: Abstract
    Description: The HUST-Grace2020 model is the latest GRACE-only gravity field solution developed at Huazhong University of Science and Technology. The model includes a set of spherical harmonic coefficients with different maximum degrees (60 and 90), and they are all unconstrained solutions. During retrieving our model, the reprocessed GRACE L1b RL03 data is used, and the newly de-aliasing product AOD1B RL06 is applied. Further details are presented in Zhou et al. (2018, 2019). This work is supported by the National Natural Science Foundation of China (No. 42074018, 41704012, 41931074, 42061134007) and National Key Research and Development Program of China (No. 2018YFC1503503, 2018YFC1503504).
    Description: Other
    Description: Parameters: product_type: gravity_field modelname: HUST-Grace2020-nLL-YYYYMM generating institute: HuaZhong University of Science and Technology earth_gravity_constant: 3.9860044150E+14 radius: 6.3781363000E+06 max_degree: LL errors: formal norm: fully_normalized tide_system: zero_tide
    Keywords: GRACE ; monthly gravity field model ; ICGEM ; geodesy ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS 〉 GEOID CHARACTERISTICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD
    Type: Dataset , Dataset
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  • 50
    Publication Date: 2023-03-03
    Description: Abstract
    Description: This dataset provides results from rheological tests of glucose syrup from two suppliers tested within the EPOS Multi-scale Laboratories (MSL) trans-national access (TNA) program 2019 at the Laboratory of Experimental Tectonics (LET), Univ. Roma TRE, Italy. Syrups Glucowheat 45/81 (GW45) and Glucowheat 60/79 (GW60) are produced by Blattmann Schweiz AG, Switzerland (2019 batch). Syrups GlucoSweet 44 (GS44) and GlucoSweet 62 (GS62) are produced by ADEA (Amidi Destrini ed Affini), Italy (2019 batch) . The four tested glucose syrups are labeled according to their DE value (dextrose equivalent value). For tested products from Blattmann Schweiz AG, the second number refers to the weight percentage of dry substance. Glucose syrup GS44 is used in full lithospheric scale analogue experiments at the Tectonic Modelling Lab (TecLab) at the University of Bern, Switzerland as a low-viscosity material simulating the asthenospheric mantle lithosphere to provide isostatic equilibration. The materials have been analyzed using a MCR301 Rheometer (Anton Paar) equipped with parallel plates geometry and rotational regime . To prevent the evaporation of the samples during the measurements, an external water-lock device has been used.
    Keywords: EPOS ; European Plate Observing System ; analogue models of geologic processes ; multi-scale laboratories ; property data of analogue modelling materials ; glucose syrup ; software tools ; force sensor ; temperature measurement ; matlab ; rheometer ; stress exponent ; viscosity ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 PLATE BOUNDARIES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 STRAIN
    Type: Dataset , Dataset
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  • 51
    Publication Date: 2023-03-06
    Description: Abstract
    Description: The dataset is an extended and updated version of the homogenized regional earthquake catalogue of the Marmara region, north-western Turkey, presented in Bohnhof et al. (2017) and Wollin et al. (2018). It is built on the regional Turkish seismicity catalogues provided by AFAD (Disaster and Emergency Management Presidency of Turkey) and KOERI (Kandilli Observatory and Earthquake Research Institute) and spans the time interval 2006-2020. All events available in these two catalogues in the wider Marmara region were combined and dublicate events removed. A total of 13812 events having at least 6 P- and/or S-picks were located using the NLLoc software (Lomax et al., 2000, 2009) in Octtree mode utilizing automatic picks (see Wollin et al., 2018 for details) for all available waveforms. The magnitude range is between M0.3 and M5.7 with time-variable magnitude of completeness and covers the area 39.70S-41.50S and 26.0E-30.65E. The full description of the data and methods is provided in the data description file.
    Keywords: seismicity ; enhanced seismicity catalog ; Sea of Marmara region ; AFAD ; KOERI ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 NEOTECTONICS
    Type: Dataset , Dataset
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  • 52
    Publication Date: 2023-03-09
    Description: Abstract
    Description: The Global Gravity-based Groundwater Product (G3P) provides groundwater storage anomalies (GWSA) from a cross-cutting combination of GRACE/GRACE-FO-based terrestrial water storage (TWS) and storage compartments of the water cycle (WSCs) that are part of the Copernicus portfolio. The data set comprises gridded anomalies of groundwater, TWS, and the WSCs glacier, snow, soil moisture and surface water bodies plus layers containing uncertainty information for the individual data products. All WSCs are spatially filtered with a Gaussian filter to be compatible with TWS. Spatial coverage is global, except Greenland and Antarctica, with 0.5-degree resolution. Temporal coverage is from April 2002 to December 2020 with monthly temporal resolution. Gridded data sets are available as NetCDF files containing variables for the parameter value as anomaly in mm equivalent water height and the parameter’s uncertainty as mm equivalent water height. The latest version of the data is visualized at the GravIS portal: http://gravis.gfz-potsdam.de/gws. From GravIS, the data is also available as area averages for several large river basins and aquifers, as well as for climatically similar regions. G3P was funded by the EU Horizon 2020 programme in response to the call LC-SPACE-04-EO-2019-2020 “Copernicus evolution – Research activities in support of cross-cutting applications between Copernicus services” under grant agreement No. 870353. --------------------------------------------------------------------------------------------- Version History: 10 March 2023: Release of Version v1.11. This is the initial release of the data.
    Keywords: Terrestrial Water Storage ; Water Balance ; Satellite Gravimetry ; Copernicus ; Groundwater ; Groundwater Storage Variations ; Mass change ; Gravity Recovery And Climate Experiment ; GRACE ; GRACE Follow-on ; GRACE-FO ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 GROUND WATER 〉 WATER TABLE ; environment 〉 natural environment 〉 terrestrial environment ; The Present
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  • 53
    Publication Date: 2023-03-10
    Description: Abstract
    Description: This data set provides a series of experiments from ring-shear tests (RST) on various materials that are used at several laboratories worldwide. The data contains the results of slide-hold-slide tests and the processed outputs of standardized ring shear tester data from related publications. Additionally, microscopy images of the materials under plain and polarized light are provided. The time dependent restrengthening of the materials is quantified using slide-hold-slide tests. This restrengthening has implications on the reactivation potential of granular shear zones in analogue models. With the provided software we first analyze the experimental data and then compare the angles and stresses needed to reactivate normal faults in the materials. We find that while healing rates are low, the majority of samples can not reactivate normal faults that are generated through extension of an analogue model.
    Keywords: Analogue Model ; Rate-and-State Friction ; Slide-Hold-Slide Test ; Basin Inversion ; Fault Reactivation ; EPOS ; multi-scale laboratories ; analogue models of geologic processes ; property data of analogue modelling materials ; deformation 〉 shearing ; EARTH SCIENCE 〉 LAND SURFACE 〉 SOILS 〉 SOIL MECHANICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 FAULT MOVEMENT ; fault ; Force sensor ; Friction coefficient ; Microspheres 〉 Glassy ; Python ; Rate-state parameters ; Ring-shear tester
    Type: Dataset , Dataset
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  • 54
    Publication Date: 2023-03-10
    Description: Abstract
    Description: The software is provided as an executable python module. The software automatically analyzes the files present in the data publication. The results are saved in the form of the images presented in the main publication. Each figure is implemented as a dedicated function that first loads the necessary data, then does some processing steps, such as curve fitting, and then plots the outputs in the desired layout. A 'main' function calls all figure functions sequentially. However, the packages is modular so that each individual plot has a standalone function which could be used with other, similarly structured data. Several submodules provide additional data for plotting, e.g. the 'groups' submodule that contains naming schemes and the densities for all samples.
    Description: TechnicalInfo
    Description: To install the package run: "python -m pip install git+https://git.gfz-potsdam.de/analab-code/granular-healing.git" To run the script run: "python -m granularhealing"
    Description: Other
    Description: License: GNU General Public License, Version 3, 29 June 2007 Copyright © 2023 Michael Rudolf Granular-Healing is free software: you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation, either version 3 of the License, or (at your option) any later version. Granular-Healing is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License for more details. You should have received a copy of the GNU General Public License along with this program. If not, see 〈http://www.gnu.org/licenses/〉.
    Keywords: EPOS ; multi-scale laboratories ; analogue models of geologic processes ; software tools ; ring shear tester ; In Situ/Laboratory Instruments 〉 Gauges 〉 RING SHEAR TESTERS ; science 〉 informatics 〉 data processing system
    Type: Software , Software
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  • 55
    Publication Date: 2023-03-13
    Description: Abstract
    Description: This data publication contains seismic waveform data of 507 earthquakes recorded during the St1 Deep Heat project in June and July 2018, where the 6.1 km deep OTN-3 well near Helsinki, Finland, was hydraulically stimulated over 49 days (Kwiatek et al., 2019). The waveforms were recorded on a surrounding seismic monitoring network consisting of 12 stations, deployed at epicentral distances between 0.6 to 8.2 km and at depths between 0.23 to 1.15 km. Each station consists of three-component, 4.5 Hz, Sunfull PSH geophones, sampling at 500 Hz. The 507 earthquakes analysed were chosen from the relocated event catalogue by Leonhardt et al. (2021a). The dataset is supplementary material to the Geophysical Research Letters research article of Holmgren et al. (2022), which applied the Empirical Green’s Function technique to examine microseismic rupture behaviour at the Helsinki site.
    Keywords: induced seismicity ; earthquake directivity ; rupture velocity ; earthquake hazard ; hydraulic stimulation ; rupture propagation ; unilateral ruptures ; bilateral ruptures ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 SEISMIC PROFILE 〉 SEISMIC BODY WAVES ; geological process 〉 seismic activity 〉 earthquake
    Type: Dataset , Dataset
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  • 56
    Publication Date: 2023-03-17
    Description: Abstract
    Description: Tourmaline-cemented magmatic-hydrothermal breccias are a major host to sulphide mineralization in the supergiant Río Blanco–Los Bronces (RB–LB) porphyry Cu-Mo district in central Chile. We made an extensive study of the chemical and boron isotopic composition of tourmaline from this district to shed light on the composition and origin of mineralizing fluids and to test the utility of tourmaline as an indicator mineral by comparing compositions from mineralized and barren breccias. Río Blanco-Los Bronces is a world-class porphyry-type Cu-Mo district of late Miocene age hosted in a granodioritic batholith and related porphyry intrusions in central Chile (33°9’ S latitude, 70°17’W longitude). The porphyry intrusions and related orebodies are distributed along a structurally-controlled NW-SE zone. Mineralization comprises quartz-sulfide veins, disseminated sulfide miner-alization in altered porphyry host rocks and disseminated sulfides in hydrothermal breccias. See Toro et al. (2012) for an overview of the geology, geochronology and mineralization in the district. Descriptions of the mineralized tourmaline breccias are given by Frikken et al. (2005) and Skewes et al. (2003). The data set provided here comprises in-situ chemical analyses of tourmaline by electron microprobe (EPMA) as well as in-situ boron-isotope analyses of tourmaline in the same samples by SIMS. Tourmaline was analysed in 12 samples including 8 from mineralized breccia bodies (Sur-Sur: 4, La Americana: 4), and 2 samples each from barren breccia and nearby granite-hosted tourmaline nodules in the Diamante area. We also give results of mass balance calculations testing the hypoth-esis of a magmatic-hydrothermal origin of the boron.
    Description: Methods
    Description: Electron microprobe (EPMA) Most samples were analyzed at the Technical University, Bergakademie in Freiberg while samples RB304 and RB306 were at the German Research Centre for Geosciences (GFZ) in Potsdam. All analyses were done on carbon-coated polished thin sections with wavelength-dispersive spetrometers, see details below. All mineral formulae were calculated by normalizing to 15 cations on the Y, Z, or T sites as implemented in the software WinTcalc (Yavuz et al., 2014). EPMA analyses in Freiberg employed a JEOL JXA-8900R instrument set at 20 kV accelerating voltage, a beam current of 12 nA, and a beam diameter of 5 microns on the sample surface. The counting times on peak were 15 s for Na, 20 s for Al, Si; 30 s for Fe, Mg; 60 s for Ti, K, V, Ca, Mn, Cr; and 90 s for F. Background counting times were half of those on the respective peak. Calibration standards used: wollastonite (Ca, Si), diopside (Mg), hematite (Fe), albite (Na), rutile (Ti), orthoclase (K, Al), fluorite (F), rhodonite (Mn), V-metal (V). The analyses at the GFZ Potsdam were carried out with a JEOL JXA 8230 electron microprobe equipped with a LaB6-cathode. The accelerating voltage was 15 kV, beam current 10 nA and the beam diameter on sample was 5 microns. Counting times on peak were 10 s for Si, K, and Na; 20 s for Al, F, Ti, Ca, Cl, Mg, Fe and Mn; background counting times were half of those on the respective peaks. Fluorine was not analysed in the GFZ session. Calibration employed the following mineral standards: orthoclase (Si, Al, K), rutile (Ti), diopside (Ca, Mg), synthetic albite (Na), hematite (Fe) and rhodonite (Mn). SIMS Boron isotope analyses employed the Cameca 1280-HR instrument at the GFZ Potsdam operated in multicollection mode with Faraday cups. Analyses were made on polished thin sections after cleaning in pure ethanol and gold coating in vacuum. The 16O- primary beam of approx. 5nA current and 13 kV energy was focused to about 5 microns on the sample surface. Secondary ions were extracted with a 10 kV potential and no offset voltage. Each analysis was preceded by a 90 s sputtering followed by 20 cycles of 10B (4 s integration time) and 11B (2 s integration) per cycle. The mass resolution M/ΔM of 2000 was more than enough to separate 11B and 10B1H masses. Instrumental mass fractionation and analytical quality were determined by repeated analyses of reference materials dravite (Harvard #108796) and schorl (Harvard #112566) described by Dyar et al. (2001) during each analytical session (see Table 3). The internal precision of each analysis (1 standard deviation / mean of 20 cycles) was typically around 0.1‰. Repeatability on the individual reference tourmalines was between 0.1 and 0.2%, and the combined 1 s.d. variability of all analyses from both reference materials was 〈0.8‰. This variability includes any matrix effect resulting from different chemical composition of the tourmalines and is taken as an estimate for the overall uncertainty. After correction for instrument mass fractionation, the 11B/10B ratios were converted to δ11B values relative to NIST SRM 951 (11B/10B = 4.04362 according to Catanzaro et al., 1970).
    Description: Other
    Description: Acknowledgements: The study was supported by the Chilean Commission for Scientific and Technological Research (CONICYT) and the German Academic Exchange Service (DAAD). We thank Thomas Seifert and Lothar Ratschbacher for support in Freiberg including expenses for field visits, sample preparation and analyses. The EPMA analyses were conducted with the help of Bernhard Schulz and Joachim Krause in Freiberg and Oona Appelt in Potsdam. The SIMS analyses in Potsdam were done with the expert help of Frederic Couffignal.
    Keywords: tourmaline ; porphyry copper ; Andes ; chemical element 〉 element of group III 〉 boron ; In Situ/Laboratory Instruments 〉 Probes 〉 ELECTRON MICROPROBES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 SIMS
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  • 57
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of engineering housekeeping data (ENG) data of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data is available from May to November 2016.
    Keywords: ELFIN-L ; Level-1 ; ENG ; Electron Losses and Fields INvestigation Onboard Lomonosov Satellite ; engineering data ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
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  • 58
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of Pierce-Rowe Magnetometer data (PRM) of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data is available from May to November 2016.
    Keywords: ELFIN-L ; Level-1 ; PRM ; Electron Losses and Fields INvestigation on board the Lomonosov satellite ; Pierce-Rowe Magnetometer data ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
    Type: Dataset , Dataset
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  • 59
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of electron particle detector (EPD) counts data of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data rate is 2 measurements per second on 8 physical electron detectors with 12 sub-channels from 21 keV to 4.7 MeV. The data is available from May to November 2016. Due to commissioning-phase and changes in the detector configuration only data from August to November 2016 is usable. Some of the electron detector channels do not provide valid or other than noise measurements. The valid channels are for 21 keV, 30 keV, 44 keV, 1.006 MeV and 1.600 MeV.
    Keywords: ELFIN-L ; Level-1 ; EPD ; Electron Particle Detector ; Electron Losses and Fields INvestigation Onboard Lomonosov Satellite ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
    Type: Dataset , Dataset
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  • 60
    Publication Date: 2023-03-20
    Description: Abstract
    Description: Gas hydrates are ice-like crystalline solids in which water molecules trap gas molecules in clathrate structures. They can preserve in low temperatures and elevated pressures and may exist in permafrost or deep marine environments. Natural gas hydrates are especially sensitive to the changes in temperature and pressure due to environmental changes. This can result in hydrate decomposition, which in turn may release enormous amounts of CH4 as the main component of natural gas hydrates. This study was an effort to use the molecular simulations for the estimation of possible gas release from the destabilization of natural gas hydrate reservoirs in response to environmental changes. The dissociation data for simple CH4 hydrates, CH4-C3H8 hydrates and CH4-C2H6-C3H8-CO2 mixed hydrates were provided by using molecular dynamics (MD) simulations. The MD simulations could provide a better understanding of the phenomena involved in the dissociation process of gas hydrates and help to explain the experimental observations. It would be one of the best molecular simulation tools for calculating time-dependent properties. The simple CH4 form structure I (sI) hydrates, while the above-mentioned binary and multicomponent gas mixtures can form structure II (sII) hydrates. Different simulation boxes were designed based on the structures and guest molecules of the gas hydrates. The simulation for CH4 hydrates was done via thermal stimulation above the ice point and depressurization below the ice point. For the mixed hydrates, the simulation data were only provided via thermal stimulation above the ice point. The dataset showed the simulation source files as well as the calculated time-dependent properties of gas hydrates upon the dissociation process. This included the simulation trajectories, gas density profiles, order parameters, ratios of large-to-small cavities, normalized rates of cavity decomposition, and gas compositions. This dataset contains the inputs/outputs of four simulation runs which include the molecular coordinate and structure (.gro file) and trajectory (.xtc file), as well as the calculated time-dependent properties (.vmd and .xls files) for each run. The simulation time and length were presented in nanoseconds (ns) and nanometers (nm), respectively. Further details on the simulation methodology, procedures, and calculations have been provided in the following sections.
    Keywords: CH4 hydrate dissociation ; Mixed gas hydrates dissociation ; Molecular dynamics simulation ; Environmental changes ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 PERMAFROST/METHANE RELEASE ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 GAS HYDRATES ; experiment 〉 simulation 〉 mathematical method ; experiment 〉 simulation 〉 modelling
    Type: Dataset , Dataset
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  • 61
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of additional adiabatic invariants (Lm, K and I) data of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data is available from May to November 2016.
    Keywords: ELFIN-L ; Level-2 ; Adiabatic Invariants ; Electron Losses and Fields INvestigation on board the Lomonosov satellite ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
    Type: Dataset , Dataset
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  • 62
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of calibrated electron particle detector (EPD) data of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data rate is 2 measurements per second on 8 physical electron detectors with 12 sub-channels from 21 keV to 4.7 MeV. The data is available from May to November 2016. Due to commissioning-phase and changes in the detector configuration only data from August to November 2016 is usable. Some of the electron detector channels do not provide valid or other than noise measurements. The valid channels are for 21 keV, 30 keV, 44 keV, 1.006 MeV and 1.600 MeV.
    Keywords: ELFIN-L ; Level-3 ; EPD ; Electron Losses and Fields INvestigation on board the Lomonosov satellite ; Electron Particle Detector ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
    Type: Dataset , Dataset
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  • 63
    Publication Date: 2023-03-20
    Description: Abstract
    Description: The objective of the Lomonosov satellite development concerns the studies of the ultra-high energy cosmic rays and fast processes in optic, X-ray and gamma-ranges which occur in the upper layers of the Earth's atmosphere and in the Universe. This dataset consists of calibrated electron particle detector (EPD) data of the ELFIN-L instrument which has been described in Shprits et al. (2018). The data rate is 2 measurements per second on 8 physical electron detectors with 12 sub-channels from 21 keV to 4.7 MeV. The data is available from May to November 2016. Due to commissioning-phase and changes in the detector configuration only data from August to November 2016 is usable. Some of the electron detector channels do not provide valid or other than noise measurements. The valid channels are for 21 keV, 30 keV, 44 keV, 1.006 MeV and 1.600 MeV.
    Keywords: ELFIN-L ; Level-2 ; EPD ; Electron Losses and Fields INvestigation on board the Lomonosov satellite ; Electron Particle Detector ; Earth Observation Satellites 〉 NOAA POES (Polar Orbiting Environmental Satellites) 〉 NOAA-19 ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 IONOSPHERE/MAGNETOSPHERE DYNAMICS 〉 MAGNETIC STORMS ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE FLUX 〉 ELECTRON FLUX ; EARTH SCIENCE 〉 SUN-EARTH INTERACTIONS 〉 SOLAR ENERGETIC PARTICLE PROPERTIES 〉 ENERGY DEPOSITION ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 SPACE WEATHER ADVISORIES 〉 GEOMAGNETIC STORM
    Type: Dataset , Dataset
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  • 64
    Publication Date: 2023-03-21
    Description: Abstract
    Description: The International Geodynamics and Earth Tide Service (IGETS) was established in 2015 by the International Association of Geodesy (IAG). IGETS continues the activities of the Global Geodynamics Project (GGP, 1997-2015) to provide support to geodetic and geophysical research activities using superconducting gravimeter (SG) data within the context of an international network. The Walferdange Underground Laboratory for Geodynamics (WULG) is located at the middle of a long labyrinth of galleries which originally have been established for the commercial extraction of gypsum. Exceptional temperature and humidity stability, the absence of water and human perturbations, distance from the ocean and easy access, were some of the motivations for initially choosing this site for instrumentation and Earth tide research. Instruments to measure the micro deformations produced by the tidal forces have been developed and tested in the Laboratory for more than 30 years. Ground deformations and earthquakes are or have been recorded continuously by means of spring gravimeters, vertical and horizontal pendulums, long base water tube tiltmeters, vertical and horizontal strain meters, short period and broad band seismometers. Meteorological parameters (temperature, humidity and atmospheric pressure), as well as radon gas emissions, are also continuously monitored in various locations within the mine. In 2000, the Minister of Research of the Grand-Duchy of Luxembourg decided to establish a new International Reference Station for Intercomparisons of Absolute Gravimeters (ISIAG). The instrumentation to support the project includes a superconducting gravimeter OSG-CT040, an absolute gravimeter FG5X-216, and other ancillary equipment necessary to support research. In January 2002, a first superconducting gravimeter was installed. The instrument was then stopped in March 2003 due to an abnormally large instrumental drift. In December 2003, it was replaced by a brand-new gravimeter with the same name and which continuously operates since that date. Absolute gravity measurements have been performed on a regular time base to calibrate the superconducting gravimeter and to estimate its instrumental drift. Since 2003, the WULG hosted three European Comparisons and one International Comparison of Absolute Gravimeters. It was the first international comparison outside the walls of the BIPM (Bureau International des Poids et Mesures) in Sèvres (France) where it had traditionally been organized for 30 years.
    Keywords: Superconducting gravimetry ; Earth tides ; Geodynamics ; geophysics ; geodesy ; hydrology ; Absolute gravimetry ; Metrology ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
    Type: Dataset , Dataset
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  • 65
    Publication Date: 2023-03-23
    Description: Abstract
    Description: Definitive digital values of the Earth's magnetic field recorded during 1991..2019 at INTERMAGNET observatories around the world. Data includes minute, hourly and daily vector values, along with observatory baseline values for quality control. Annual means are also included. All data is included on the single downloadable archive files. This is the 28th annual publication in the series. Some national data institutions may have related DOIs that describe subsets of the data. These DOIs are shown under "Related DOIs to be quoted". For more information on the data formats used in this publication and the technical standards used to create the data, please refer to the INTERMAGNET Technical Manual and the Technical note TN6 "INTERMAGNET Definitive One-second Data Standard".
    Description: Methods
    Description: Geomagnetic data is recorded and quality controlled at the institutions responsible for each observatory. Before becoming a member of INTERMAGNET, institutes must make a detailed submission for each observatory that is to join. This submission is verified by a committee in INTERMAGNET before the observatory is admitted. Only data from INTERMAGNET members is published by INTERMAGNET. Each annual definitive data set is checked for quality by a team of data checkers in INTERMAGNET before the data is admitted to the series for that year.
    Description: Other
    Description: The International Real-time Magnetic Observatory Network (INTERMAGNET) is the global network of observatories, monitoring the Earth's magnetic field. The INTERMAGNET programme exists to establish a global network of cooperating digital magnetic observatories, adopting modern standard specifications for measuring and recording equipment, in order to facilitate data exchange and the production of geomagnetic products in close to real time. INTERMAGNET also coordinates the publication of quality-controlled, definitive geomagnetic data from its affiliated observatories.
    Keywords: definitive data ; INTERMAGNET ; geomagnetism ; magnetism ; observatory ; definitive ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMAGNETISM ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 GEOLOGICAL ADVISORIES 〉 GEOMAGNETISM ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 GEOMAGNETIC STATIONS
    Type: Dataset , Dataset
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  • 66
    Publication Date: 2023-03-26
    Description: Abstract
    Description: This is an Arctic-delta reduced-complexity model that can reproduce the 2-m ramp feature observed in most Arctic deltas. The model is built by first reconstructing from published descriptions of the DeltaRCM-Arctic model (Lauzon et al., GRL, 2019), which is, in turn, based on DeltaRCM by Liang et al. (Esurf, 2015). All the modifications and refinements leading to this model (ArcDelRCM.jl) are detailed in a manuscript submitted to Earth Surface Dynamics journal for publication (Chan et al., 2022: esurf-2022-25). Options are retained to run this model with the "DeltaRCM-Arctic" (reconstruction) setting. The code is written purely in Julia language.
    Description: Other
    Description: MIT License Copyright (c) 2020 Ngai-Ham (Erik) Chan Permission is hereby granted, free of charge, to any person obtaining a copy of this software and associated documentation files (the "Software"), to deal in the Software without restriction, including without limitation the rights to use, copy, modify, merge, publish, distribute, sublicense, and/or sell copies of the Software, and to permit persons to whom the Software is furnished to do so, subject to the following conditions: The above copyright notice and this permission notice shall be included in all copies or substantial portions of the Software. THE SOFTWARE IS PROVIDED "AS IS", WITHOUT WARRANTY OF ANY KIND, EXPRESS OR IMPLIED, INCLUDING BUT NOT LIMITED TO THE WARRANTIES OF MERCHANTABILITY, FITNESS FOR A PARTICULAR PURPOSE AND NONINFRINGEMENT. IN NO EVENT SHALL THE AUTHORS OR COPYRIGHT HOLDERS BE LIABLE FOR ANY CLAIM, DAMAGES OR OTHER LIABILITY, WHETHER IN AN ACTION OF CONTRACT, TORT OR OTHERWISE, ARISING FROM, OUT OF OR IN CONNECTION WITH THE SOFTWARE OR THE USE OR OTHER DEALINGS IN THE SOFTWARE.
    Keywords: Arctic Deltas ; Lena Delta ; 2-m Ramp ; Bottom-fast ice ; Bed-fast ice ; Reduced-complexity Model ; EARTH SCIENCE 〉 CRYOSPHERE 〉 SEA ICE 〉 ICE DEPTH/THICKNESS ; EARTH SCIENCE 〉 CRYOSPHERE 〉 SNOW/ICE 〉 PERMAFROST ; EARTH SCIENCE 〉 LAND SURFACE 〉 FROZEN GROUND 〉 ACTIVE LAYER ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 FLUVIAL LANDFORMS 〉 DELTAS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 FLUVIAL PROCESSES 〉 SEDIMENT TRANSPORT ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 GLACIAL PROCESSES 〉 FREEZE/THAW
    Type: Software , Software
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  • 67
    Publication Date: 2023-03-27
    Description: Abstract
    Description: This data publication is supplementary to a study on the effect of large boulders and bedrock fracture patterns on hillslope denudation rates in the Chilean Coastal Cordillera, by Lodes et al. (submitted). Hillslope denudation rates are primarily determined by tectonic uplift rates, but landscape morphology is also controlled by climate and lithological properties such as bedrock fractures. Fracture patterns can influence the locations of ridges and valleys in landscapes through lowering surface grain sizes in fractured areas, and therefore the residence time of fractured hillslope material, dictating differential denudation rates. In this project, we used 10Be cosmogenic nuclide analysis to quantify the denudation rates of fractured bedrock, boulders, and soil on hillslopes, and compared the orientations of surrounding streams and faults, to understand the effects of fracturing and faulting on denudation rates, fluvial incision, and grain size in three field sites along a climate gradient in the Chilean Coastal Cordillera. In the humid and semi-arid climate zones, we found that denudation rates for unfractured bedrock and large hillslope boulders (10 to 15 m Myr-1) are lower than for soil (15 to 20 m Myr-1), indicating that exposed bedrock and boulders retard hillslope denudation rates. In the mediterranean climate zone, hillslope denudation rates are higher (40-140 m Myr-1) and show a less consistent pattern, likely due to steeper slopes. LiDAR-derived stream orientations support a fracture-control on landscape denudation in the three field sites, which we link with fracture density. Together, our results thus provide new insights into how fracture patterns can dictate topographic highs and valleys through grain size reduction. The main objective of this data publication is to provide our 10Be dataset which we used to calculate denudation rates for bedrock, boulders, and soils.
    Description: Methods
    Description: We conducted fieldwork in Chile in February 2019 and March 2020. We collected 32 samples from bedrock, boulders, and topsoil in three field areas (Nahuelbuta National Park, La Campana National Park, and Private Reserve Santa Gracia) for cosmogenic 10Be analysis. A detailed description of the field areas can be found in Lodes et al. (submitted). We collected bedrock samples by chipping off and amalgamating 10-15 pieces (~25 cm2 and 〈2cm thick) of bedrock in an area of ~20 m x 20 m. Boulder samples consist of similarly-size chips from 10-15 different boulders of similar size, from an area of ~40 m x 40 m, depending on the abundance of boulders. We collected soil samples from the area surrounding the sampled boulders. The samples are assigned with IGSNs, which are listed in the accompanying data table 2022-004_Lodes-et-al_Data.
    Keywords: 10Be ; cosmogenic radionuclides ; geomorphology ; fractures ; landscape morphology ; tectonic geomorphology ; erosion ; denudation ; boulders ; hillslopes ; EARTH SCIENCE 〉 LAND SURFACE 〉 GEOMORPHOLOGY 〉 FLUVIAL LANDFORMS/PROCESSES ; EARTH SCIENCE 〉 LAND SURFACE 〉 GEOMORPHOLOGY 〉 TECTONIC LANDFORMS/PROCESSES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES ; land 〉 geomorphic process 〉 erosion ; science 〉 geography 〉 geomorphology
    Type: Dataset , Dataset
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  • 68
    Publication Date: 2023-03-29
    Description: Abstract
    Description: High resolution daylight photos with contour lines of the surface topography of moraine study plots with the dimensions (4m x 6m). The photos were taken in August 2018 in the proglacial area of the Steingletscher. Two photos show plots on a moraine that turned ice-free in 1860, three photos show plots that turned ice-free in 1990.
    Keywords: high-resolution photo ; moraine ; soil surface ; terrain ; chronosequence ; EARTH SCIENCE 〉 LAND SURFACE 〉 LANDSCAPE 〉 LANDSCAPE PROCESSES
    Type: Dataset , Dataset
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  • 69
    Publication Date: 2023-03-29
    Description: Abstract
    Description: SAM ("Simplified Analytical Model") is a MatLab-based software that allows for fast and flexible simulations of three-dimensional dyke pathways in an elastic medium. The model was first introduced in "Mechanical modeling of pre-eruptive magma propagation scenarios at calderas" (Mantiloni, L. et al. 2023). In SAM, dykes are modelled as penny-shaped cracks of fixed radius, opening against the local direction of the least-compressive principal stress. The direction of propagation is determined by the gradient of the external stress normal to the crack's plane and the buoyancy force of the magma filling the dyke, calculated at a set of observation points along the crack's tipline. The model can also include a uniform internal pressure within the dyke and compute the stress intensity factor along the crack's tipline, comparing it to the fracture toughness of the host rock to determine if the dyke will advance. SAM needs a model for the stress field of the host rock as input, as well as magma and rock densities, rock elastic properties, the dyke's radius and the number of observation points. The model may be applied to simulate dyke pathways in realistic volcanic settings with different stress sources, and can perform large numbers of simulations in little time. The model does not, however, account for any viscous flow of magma within the dyke, nor the velocity of dyke propagation. Dykes cannot change shape or area during the propagation, and are always bound to be oriented normally to the local least-compressive principal stress axis. This repository also includes data and parameters of the synthetic scenarios discussed in "Mechanical modeling of pre-eruptive magma propagation scenarios at calderas".
    Keywords: Dyke Propagation Modeling ; Hydrofractures ; Stress Modelling ; Magma Propagation ; Calderas ; Volcanoes ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 ERUPTION DYNAMICS 〉 MAGMA SPEED/FLOW ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 VOLCANO PREDICTIONS ; geological process 〉 volcanism
    Type: Software , Software
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  • 70
    Publication Date: 2023-03-31
    Description: Abstract
    Description: This data repository contains the IGMAS+ (Gotze and Lahmeyer, 1988; Schmidt et al., 2011, 2020) files of the four end-member structural and density models used to analyze the rift architecture of the Red Sea. The user can directly open the files in IGMAS+ (https://igmas.git-pages.gfz-potsdam.de/igmas-pages/, accessed 12.08.2022) to explore the gravity response of these configurations. The end-member scenarios include two end-type margin architectures following Huismans and Beaumont (2011): Type I - outlined by narrow regions (less than about 100 km wide) of thinned continental crust and exhumed (and serpentinized) continental lithospheric mantle along the continent-ocean transition, and Type II - outlined by (ultra)wide regions (up to 500 km) of thin continental crust and the removal of the lithospheric mantle. In addition, we include two options for distribution of oceanic crust in the Red Sea: limited - confined only to regions of magnetic stripes following Schettino et al. (2016), and extended - in which oceanic crust is available in vast areas within the basin, following Augustin et al. (2021).
    Keywords: Red Sea ; Lithospheric configuration ; Rift architecture ; 3D gravity models ; EARTH SCIENCE ; EARTH SCIENCE 〉 OCEANS 〉 MARINE GEOPHYSICS 〉 MARINE GRAVITY FIELD ; EARTH SCIENCE 〉 SOLID EARTH ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS
    Type: Model , Model
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  • 71
    Publication Date: 2023-04-03
    Description: Methods
    Description: In die Datenbank aufgenommen, wurden jene Personen, die ab 1949 eine Professur in Geographie an einer deutschsprachigen Hochschule mit Promotionsrecht innehatten (nicht aufgenommen wurden: Assistenz-, Honorar-, Apl.-, Vertretungs- und Juniorprofessor:innen). Berücksichtigt wurden nicht nur Universitäten, sondern auch Pädagogische Hochschulen, sofern diese über Promotionsrecht verfügten. Für die Zusammenstellung der GEOprof-Database wurden ganz unterschiedliche Quellen herangezogen: Für die Erfassung der derzeitigen Hochschullehrer:innen konnte relativ problemlos auf deren Internetauftritte zurückgegriffen werden; je weiter wir jedoch in die Vergangenheit zurückgingen, desto vielfältiger wurden die Datenfundorte. Wichtige Quellen waren: Das Geographische Taschenbuch, Kürschners Deutscher Gelehrten-Kalender, der Personalia-Teil des Rundbriefs Geographie, das Mitgliederverzeichnis des VGDH, diverse Festschriften und Nachrufe, Zeitungsmeldungen, Webarchive und archivierte Vorlesungsverzeichnisse sowie schriftliche oder mündliche Auskünfte von UniversitätsarchivarInnen oder den Professor:innen selbst. Außerdem hat uns Heinz Peter Brogiato (IfL, Leipzig) dankenswerterweise die von ihm erstellte Liste ehemaliger Geographie-Professor:innen (bis 1960) zur Verfügung gestellt. Einen herzlichen Dank an alle, die uns unterstützt haben!
    Description: Other
    Description: Von Herbst 2018 bis zum Sommer 2021 wurde am Lehrstuhl für Anthropogeographie der Universität Passau die GEOprof-Database erstellt. Bei dieser Datenbank handelt es sich um die erste vollständige Zusammenstellung der Professor:innenschaft der deutschsprachigen Geographie (Deutschland. Österreich, deutschsprachige Schweiz und Luxemburg (ab 2006). Die hier zur Verfügung gestellte GEOprof-Database ist für die historiographische Erforschung der deutschsprachigen Geographie von großem Wert; sie kann Basis und Ausgangspunkt für die Bearbeitung unterschiedlicher fachhistorischer und wissenschaftssoziologischer Untersuchungen sein. In der Datenbank finden sich Informationen zur akademischen Biographie der gesamten Geographieprofessor:innenschaft inklusive der Forschungschwerpunkte, der beruflichen Stationen seit dem ersten Ruf sowie der Denomination der jeweiligen Professur.
    Description: Abstract
    Description: The GEOprof-Database was developed at the Chair of Human Geography at the University of Passau between autumn 2018 and summer 2021. The development of the database was part of a research project funded by the German Research Council (DFG). The GEOprof-Database is the first complete compilation of the professorate of German-speaking geography (Germany. Austria, German-speaking Switzerland and Luxembourg). The database includes basic information on all full professors from 1949 to 2021. The GEOprof-Database is of great value for historiographical research of German-speaking geography. It can be the basis and starting point of different historical and sociological studies of the discipline. The database contains information on the academic biography of the entire geography professorate.
    Keywords: Historische Geographie ; Geographiegeschichte ; Wissenschaftsforschung ; Disziplinentwicklung ; Professorendatenbank ; Professorenschaft ; science 〉 geography
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  • 72
    Publication Date: 2023-04-06
    Description: Abstract
    Description: The atmospheric concentration of CO2 at which global glaciation (snowball) bifurcation occurs, changes throughout Earth's history, most notably because of the slowly increasing solar luminosity. Quantifying this critical CO2 concentration is not only interesting from a climate dynamics perspective, but also an important prerequisite for understanding past Snowball Earth episodes as well as the conditions for habitability on Earth and other planets. Here we use the coupled climate model CLIMBER-3α in an Aquaplanet configuration to scan for the Snowball bifurcation point for time slices spanning the last 4 billion years, thus quantifying the time evolution of the bifurcation and identifying a qualitative shift in critical state dynamics.
    Description: Methods
    Description: To scan for the Snowball bifurcation for more than a dozen time slices throughout Earth’s history, we use the relatively fast Earth-system model of intermediate complexity CLIMBER-3α. It consists of a modified version of the ocean general circulation model (OGCM) MOM3 with a horizontal resolution of 3.75◦× 3.75◦ and 24 vertical levels, a dynamic/thermodynamic sea-ice model the same horizontal resolution and a fast statistical-dynamical atmosphere model with a coarse horizontal resolution of 22.5◦ in longitude and 7.5◦ in latitude. The sea-ice model explicitly takes into account sea-ice dynamics, a factor which has been found to be of crucial importance for the Snowball bifurcation. The effects of snow cover on sea ice are explicitly taken into account. The main limitations of the model relate to its simplified atmosphere component. For more details see the corresponding paper.
    Keywords: paleoclimate ; Snowball Earth ; global glaciation ; snowball bifurcation ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 GLACIATION ; EARTH SCIENCE SERVICES 〉 MODELS 〉 COUPLED CLIMATE MODELS
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  • 73
    Publication Date: 2023-04-11
    Description: Abstract
    Description: The present dataset is a comprehensive earthquake catalogue for the Northern Chile subduction zone forearc covering the period 2007-2021, determined from IPOC seismic station data (GFZ and CNRS-INSU 2006; https://doi.org/10.14470/pk615318) plus some auxiliary stations (IPOC = Integrated Plate Boundary Observatory Chile; http://www.ipoc-network.org). The method of automatized earthquake catalogue retrieval, the different relocation steps as well as the different earthquake class labels, and the structures outlined by the seismicity are described in detail in Sippl et al. (2023). The catalogue builds on the one from Sippl et al. (2018; https://doi.org/10.5880/GFZ.4.1.2018.001), but uses a slightly deviating parameter set and a new event category. The columns of the data files are: year, month, day, hour, minute, second, latitude [dec. degrees], longitude [dec. degrees], depth [km], magnitude [ML], identifier The identifier term provides a first-order spatial classification of the seismicity, an explanation is given in Sippl et al. (2023).
    Keywords: IPOC ; Chile ; Integrated Plate Observatory Chile ; EARTH SCIENCE ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 PLATE BOUNDARIES
    Type: Dataset , Dataset
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  • 74
    Publication Date: 2023-04-11
    Description: Methods
    Description: Under the coordination of the German Research Centre for Geosciences GFZ the first European onshore CO2 storage project was initiated in 2004 at Ketzin, approximately 25 km west of Berlin, Germany. About 67 kt of CO2 (purity 〉 99.9%) were injected into a saline aquifer from June 2008 until August 2013. All project stages were accompanied by a comprehensive monitoring and modelling program, focusing on the investigation of the processes involved and to assure leakage-free CO2 injection and save geological storage. Hence, methods from different geoscientific disciplines were applied, targeting the reservoir itself, the cap rock, the above-zone and the surface (Martens et al. 2015, Wipki et al. 2016). Here we report on the results of the long-term surface monitoring with continuous soil CO2 flux measurements. A profound and extensive database of measurements performed before injection started serves to interpret data during and after CO2 injection (Zimmer et al. 2011). As the CO2 flux measurements reflect the specific site conditions, which can vary locally and over time, trends must be interpreted carefully. After an exploration phase in 2004 and drilling of the first wells in 2007, CO2 was injected between 2008 and 2013 into Upper Triassic sandstones at a depth of 630 to 650 m. This reservoir is overlain by more than 165 m of shaley cap rocks. The site itself is located at the southern flank of the Roskow-Ketzin double-anticlinal structure (Martens et al. 2014, Förster et al. 2006, Förster et al. 2009) and the stored CO2 mainly migrated in northern to western direction (Wipki et al. 2016 ). Additionally, soil profiles of 70 cm depth were studied for their structure and carbon and nitrogen concentrations. The results helped to explain the spatial variations of the soil CO2 fluxes at the different locations (Zimmer et al. 2011). However, as most of the sampling positions are located next to agricultural roads and fields, an influence of used fertilizers and arable farming on the soil structure, chemical composition and the soil biology cannot be ruled out.
    Keywords: soil CO2 flux ; Ketzin CO2 storage pilot site ; CO2 storage ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC CHEMISTRY 〉 CARBON AND HYDROCARBON COMPOUNDS 〉 CARBON DIOXIDE ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 WATER QUALITY/WATER CHEMISTRY 〉 CARBON DIOXIDE
    Type: Dataset , Dataset
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  • 75
    Publication Date: 2023-04-18
    Description: Abstract
    Description: As the negative impacts of hydrological extremes increase in large parts of the world, a better understanding of the drivers of change in risk and impacts is essential for effective flood and drought risk management and climate adaptation. However, there is a lack of comprehensive, empirical data about the processes, interactions and feedbacks in complex human-water systems leading to flood and drought impacts. To fill this gap, we present an IAHS Panta Rhei benchmark dataset containing socio-hydrological data of paired events, i.e. two floods or two droughts that occurred in the same area (Kreibich et al. 2017, 2019). The contained 45 paired events occurred in 42 different study areas (in three study areas we have data on two paired events), which cover different socioeconomic and hydroclimatic contexts across all continents. The dataset is unique in covering floods and droughts, in the number of cases assessed and in the amount of qualitative and quantitative socio-hydrological data contained. References to the data sources are provided in 2023-001_Kreibich-et-al_Key_data_table.xlsx where possible. Based on templates, we collected detailed, review-style reports describing the event characteristics and processes in the case study areas, as well as various semi-quantitative data, categorised into management, hazard, exposure, vulnerability and impacts. Sources of the data were classified as follows: scientific study (peer-reviewed paper and PhD thesis), report (by governments, administrations, NGOs, research organisations, projects), own analysis by authors, based on a database (e.g. official statistics, monitoring data such as weather, discharge data, etc.), newspaper article, and expert judgement. The campaign to collect the information and data on paired events started at the EGU General Assembly in April 2019 in Vienna and was continued with talks promoting the paired event data collection at various conferences. Communication with the Panta Rhei community and other flood and drought experts identified through snowballing techniques was important. Thus, data on paired events were provided by professionals with excellent local knowledge of the events and risk management practices.
    Keywords: hydrological extremes ; risk dynamics ; human-flood system ; human-drought system ; socio-hydrology ; risk management ; flood ; drought ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 ENVIRONMENTAL GOVERNANCE/MANAGEMENT 〉 WATER MANAGEMENT ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 DROUGHTS ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 FLOODS ; EARTH SCIENCE SERVICES 〉 DATA ANALYSIS AND VISUALIZATION ; environmental assessment 〉 environmental risk assessment
    Type: Dataset , Dataset
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  • 76
    Publication Date: 2023-04-12
    Description: Methods
    Description: In die Datenbank aufgenommen, wurden jene Personen, die ab 1949 eine Professur in Geographie an einer deutschsprachigen Hochschule mit Promotionsrecht innehatten (nicht aufgenommen wurden: Assistenz-, Honorar-, Apl.-, Vertretungs- und Juniorprofessor:innen). Berücksichtigt wurden nicht nur Universitäten, sondern auch Pädagogische Hochschulen, sofern diese über Promotionsrecht verfügten. Für die Zusammenstellung der GEOprof-Database wurden ganz unterschiedliche Quellen herangezogen: Für die Erfassung der derzeitigen Hochschullehrer:innen konnte relativ problemlos auf deren Internetauftritte zurückgegriffen werden; je weiter wir jedoch in die Vergangenheit zurückgingen, desto vielfältiger wurden die Datenfundorte. Wichtige Quellen waren: Das Geographische Taschenbuch, Kürschners Deutscher Gelehrten-Kalender, der Personalia-Teil des Rundbriefs Geographie, das Mitgliederverzeichnis des VGDH, diverse Festschriften und Nachrufe, Zeitungsmeldungen, Webarchive und archivierte Vorlesungsverzeichnisse sowie schriftliche oder mündliche Auskünfte von UniversitätsarchivarInnen oder den Professor:innen selbst. Außerdem hat uns Heinz Peter Brogiato (IfL, Leipzig) dankenswerterweise die von ihm erstellte Liste ehemaliger Geographie-Professor:innen (bis 1960) zur Verfügung gestellt. Einen herzlichen Dank an alle, die uns unterstützt haben!
    Description: Other
    Description: Bei der GEOprof-Database, die seit 2018 am Lehrstuhl für Anthropogeographie der Universi-tät Passau entwickelt wird, handelt es sich um die erste vollständige Zusammenstellung der Professor:innenschaft der deutschsprachigen Geographie (Deutschland. Österreich, deutschsprachige Schweiz und Luxemburg (ab 2006). Die hier zur Verfügung gestellte GEOprof-Database ist für die historiographische Erforschung der deutschsprachigen Geographie von großem Wert; sie kann Basis und Ausgangspunkt für die Bearbeitung unterschiedlicher fachhistorischer und wissenschaftssoziologischer Untersu-chungen sein. In der Datenbank finden sich Informationen zur akademischen Biographie der gesamten Geographieprofessor:innenschaft inklusive der Forschungsschwerpunkte, der be-ruflichen Stationen seit dem ersten Ruf sowie der Denomination der jeweiligen Professur. Ab Herbst 2022 erfolgten eine umfassende Aktualisierung und Erweiterung der Datenbank (V.2.0). Neuenthalten sind nun auch Informationen über die Promotion der jeweiligen Professor:innen (Titel der Dissertation, Betreuer:innen sowie Ort und Jahr der Promotion).
    Description: Abstract
    Description: The GEOprof-Database was developed at the Chair of Human Geography at the Uni-versity of Passau between autumn 2018 and spring 2023. The development of the database was part of a research project funded by the German Research Council (DFG) (No. 249237273). The GEOprof-Database is the first complete compilation of the professorate of German-language geography (Germany. Austria, German-speaking Switzerland and Luxem-bourg). The database includes basic information on all full professors from 1949 to 2022. The GEOprof-Database is of great value for historiographical research of German-language geography. It can be the basis and starting point of different historical and sociological stud-ies of the discipline. The database contains information on the academic biography of the entire geography professorate. In 2022, a comprehensive update (V.2.0) and expansion was carried out. Newly included in the database are information about the professors’ doctoral disserta-tions (dissertation’s title, year, supervisors & name of university).
    Keywords: Historische Geographie ; Geographiegeschichte ; Wissenschaftsforschung ; Disziplinentwicklung ; Professorendatenbank ; Professorenschaft ; EARTH SCIENCE ; science 〉 geography
    Type: Dataset , Dataset
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  • 77
    Publication Date: 2023-04-20
    Description: Abstract
    Description: This dataset provides the surface velocity fields derived with MatPIV (open-source Matlab toolbox for Particle Image Velocimetry; Sveen 2004) of three seismotectonic analog models (e.g., Rosenau et al., 2017) performed to investigate the role of geometry and friction of a single subducting seamount on the seismogenic behavior of the megathrust. Model 1 has a seamount covered by sandpaper (i.e., high friction) that is placed at 1/2 of the trench-parallel length of the seismogenic zone. Model 3 has the same geometry of model 1, but the seamount is in direct contact with the gelatin (i.e., not covered by sandpaper, hence low friction). Model 5 has a low friction patch (i.e., no geometry) that is placed again at 1/2 of the trench-parallel length of the seismogenic zone. Together with the surface velocity fields, we also provide Matlab scripts for visualization. A more detailed description of the experimental setup, configuration of the models and materials can be found in Menichelli et al. (submitted), to which this dataset is supplementary. Our seismotectonic models represent a downscaled subduction zone (1 cm in the model corresponds to 6.4 km in nature; Rosenau et al., 2017). The experimental setup consists of a 60 x 34 cm2 Plexiglass box with a 10°-dipping aluminum basal plate that moves downward with a constant velocity of 0.01 cm/s, analog of the subducting plate. The overriding plate is represented by an elastic wedge of 2.5 wt% pigskin gelatin at T = 10 °C (Di Giuseppe et al., 2009). The seismogenic zone of the megathrust is simulated using a rectangular sandpaper patch (Corbi et al., 2013), with a downdip width of 16 cm and located 31 and 47 cm from the backstop. This corresponds to a 100-km-wide seismogenic zone extending over a depth interval between 15 and 34 km. The updip and down dip aseismic regions of the megathrust are simulated by plastic sheets that are fixed on the setup frame and not subject to subduction (Corbi et al., 2013). A 3D-printed PLA seamount is placed on the seismogenic zone (e.g., Van Rijsingen et al., 2019). The seamount has a height of 6.28 mm and a diagonal length of 94 mm, corresponding to 4 km and 60 km in nature, respectively. These dimensions scale well-known seamounts, such as the Joban Seamount chain in the Japan Trench or the Louisville seamount chain in the Tonga-Kermadec Trench. Experiments were monitored with a CCD camera that acquired a sequence of high-resolution top-view images (1600 x 1200 pixels2, 8 bit, 256 gray levels) at 7.5 fps for the entire duration of the experiment (i.e., ca. 24 minutes). Images are processed with Particle Image Velocimetry (PIV; Adam et al., 2005) using the open-source Matlab toolbox MatPIV (Sveen, 2004). MatPIV provides the velocity field between two consecutive frames, measured at the surface of the model. The velocity field was then used as input to identify analog seismic events using the open-source Matlab function findpeak. The threshold used was 0.1 cm/s. Once earthquakes were identified, we derived their source parameters such as seismic slip, magnitude, and recurrence time following Corbi et al. (2017) and van Rijsingen et al. (2019).
    Keywords: EPOS ; multi-scale laboratories ; analogue models of geologic processes ; analogue modelling results ; software tools ; PIV
    Type: Dataset , Dataset
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  • 78
    Publication Date: 2023-04-21
    Description: Abstract
    Description: Version History: 15 June 2020: Initial release of the data. Note that the initial version number is 0002 in order to reflect the consistent data processing of this data set and Version 0002 of the data set Dahle & Murböck (2019, http://doi.org/10.5880/GFZ.GRAVIS_06_L2B). --------------------------------------------------------------------------------------------- Post-processed GRACE/GRACE-FO spherical harmonic coefficients of COST-G RL01 Level-2 GSM products representing an estimate of Earth's gravity field variations during the specified timespan. Post-processing steps comprise: (1) subtraction of a long-term mean field; (2) optionally, decorrelation and smoothing with VDK filter (anisotropic filter taking the actual error covariance information of the underlying GSM coefficients into account, see Horvath et al. (2018)); (3) replacement of coefficients C20, C30 (only for the months starting from 2016/11 and later), C21 and S21 and its formal standard deviations by values estimated from a combination of GRACE/GRACE-FO and Satellite Laser Ranging (SLR); (4) subtraction of linear trend caused by Glacial Isostatic Adjustment (GIA) as provided by a numerical model; (5) insertion of geocenter coefficients (C10, C11, S11); and (6) removal of estimated aliased signal of the S2 tide (161 days period). These coefficients represent signals caused by water mass redistribution over the continents and in the oceans. These post-processed GRACE/GRACE-FO GSM products are denoted as Level-2B products. There are multiple variants of Level-2B products available that differ by the characteristics of the anisotropic filter applied. These variants are distinguishable by the following strings in the product file names: - 'NFIL': Level-2B product is not filtered - 'VDK1': Level-2B product is filtered with VDK1 - 'VDK2': Level-2B product is filtered with VDK2 - 'VDK3': Level-2B product is filtered with VDK3 - 'VDK4': Level-2B product is filtered with VDK4 - 'VDK5': Level-2B product is filtered with VDK5 - 'VDK6': Level-2B product is filtered with VDK6 - 'VDK7': Level-2B product is filtered with VDK7 - 'VDK8': Level-2B product is filtered with VDK8 The individual auxiliary data sets and models used during the post-processing steps mentioned above are provided as well (in the aux_data folder): - 'GRAVIS-2B_2002095-2020091_GFZOP_0600_NFIL_0002.gz': Long-term mean field calculated as unweighted average of the 183 available GFZ RL06 GSM products in the period from 2002/04 up to and including 2020/03. - 'GRAVIS-2B_COSTG_GRACE+SLR_LOW_DEGREES_0002.dat': time series of coefficients C20, C30, C21 and S21 estimated from a combination of GRACE/GRACE-FO and SLR - 'GRAVIS-2B_GIA_ICE-6G_D_VM5a_0002.gz': Model from Peltier et al. (2018) for subtraction of linear trend caused by GIA - 'GRAVIS-2B_COSTG_GEOCENTER_0002.dat': Time series with geocenter coefficients estimated from COST-G RL01 Further information about the Level-2B products and the auxiliary data is provided in the header of the corresponding data files.
    Keywords: Gravity Recovery And Climate Experiment (GRACE) ; GRACE Follow-on (GRACE-FO) ; Level-2 ; Level-2B ; SHM ; Spherical Harmonic Model ; Gravitational Field ; GSM ; Geopotential ; Gravity Field ; Mass ; Mass Transport ; Total Water Storage ; Time Variable Gravity ; Mass Balance ; Gravity Anomaly ; Satellite Geodesy ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITATIONAL FIELD ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
    Type: Dataset , Dataset
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  • 79
    Publication Date: 2023-04-21
    Description: Abstract
    Description: Version History:15 June 2020:Initial release of the data. Note that the initial version number is 0002 in order to reflect the consistent data processing of this data set and Version 0002 of the data set Dobslaw et al. (2019, http://doi.org/10.5880/GFZ.GRAVIS_06_L3_OBP).---------------------------------------------------------------------------------------------GRACE/GRACE-FO Level-3 product based on COST-G RL01 Level-2B products (Dahle & Murböck, 2020) representing Ocean Bottom Pressure (OBP) variations provided at 1° latitude-longitude grids as defined over ocean areas. The OBP grids are provided in NetCDF format divided into yearly batches. The files each contain seven different variables:1) 'barslv': gravity-based barystatic sea-level pressure2) 'std_barslv': gravity-based barystatic sea-level pressure uncertainties3) 'resobp': gravity-based residual ocean circulation pressure resobp4) 'std_resobp': gravity-based residual ocean circulation pressure uncertainties5) 'leakage': apparent gravity-based bottom pressure due to continental leakage6) 'model_ocean': background-model ocean circulation pressure7) 'model_atmosphere': background-model atmospheric surface pressureThese Level-3 products are visualized at GFZ's web portal GravIS (http://gravis.gfz-potsdam.de). Link to data products: ftp://isdcftp.gfz-potsdam.de/grace/GravIS/COST-G/Level-3/OBP
    Keywords: Gravity Recovery And Climate Experiment (GRACE) ; GRACE Follow-on (GRACE-FO) ; Level-3 ; Mass ; Mass Transport ; Ocean Bottom Pressure ; Time Variable Gravity ; Mass Balance ; Satellite Geodesy ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE
    Language: English
    Type: Dataset , Dataset
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  • 80
    Publication Date: 2023-04-21
    Description: Abstract
    Description: Version History:15 June 2020:Initial release of the data. Note that the initial version number is 0002 in order to reflect the consistent data processing of this data set and Version 0002 of the data set Sasgen et al. (2019, http://doi.org/10.5880/GFZ.GRAVIS_06_L3_ICE).---------------------------------------------------------------------------------------------GRACE/GRACE-FO Level-3 products based on COST-G RL01 Level-2B products (Dahle & Murböck, 2020) representing ice-mass changes for the Antarctic Ice Sheet (AIS) and the Greenland Ice Sheet (GIS). The ice-mass changes are provided both as basin average product and as gridded product.Basin-average ice-mass changes are obtained using the inversion procedure based on a forward modelling approach as described in Sasgen et al. (2013) for the AIS and Sasgen et al. (2012) for the GIS.Gridded ice-mass changes are provided at polar-stereographic grids with a grid spacing of 50 x 50 km^2. The applied algorithm is based on tailored sensitivity kernels (Groh & Horwath, 2016), and has also been used to generate gravimetric mass balance products within the ESA Climate Change Initiative (CCI) projects for the AIS and the GIS.These Level-3 products are visualized at GFZ's web portal GravIS (http://gravis.gfz-potsdam.de).Link to data products: ftp://isdcftp.gfz-potsdam.de/grace/GravIS/COST-G/Level-3/ICE
    Keywords: Gravity Recovery And Climate Experiment (GRACE) ; GRACE Follow-on (GRACE-FO) ; Level-3 ; Mass ; Mass Transport ; Ice-mass Change ; Time Variable Gravity ; Antarctic Mass Balance ; Greenland Mass Balance ; Sea-level Change ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE
    Language: English
    Type: Dataset , Dataset
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  • 81
    Publication Date: 2023-04-21
    Description: Abstract
    Description: Version History:15 June 2020:Initial release of the data. Note that the initial version number is 0002 in order to reflect the consistent data processing of this data set and Version 0002 of the data set Boergens et al. (2019, http://doi.org/10.5880/GFZ.GRAVIS_06_L3_TWS).---------------------------------------------------------------------------------------------GRACE/GRACE-FO Level-3 product based on COST-G RL01 Level-2B products (Dahle & Murböck, 2020) representing Terrestrial Water Storage (TWS) anomalies provided at 1° latitude-longitude grids as defined over all continental regions except Greenland and Antarctica. The TWS anomaly grids are provided in NetCDF format divided into yearly batches. The files each contain four different variables:1) 'tws': gravity-based TWS2) 'std_tws': gravity-based TWS uncertainties3) 'leakage': spatial leakage contained in TWS4) 'model_atmosphere': background model atmospheric massThese Level-3 products are visualized at GFZ's web portal GravIS (http://gravis.gfz-potsdam.de). Link to data products: ftp://isdcftp.gfz-potsdam.de/grace/GravIS/COST-G/Level-3/TWS
    Keywords: Gravity Recovery And Climate Experiment (GRACE) ; GRACE Follow-on (GRACE-FO) ; Level-3 ; Mass ; Mass Transport ; Total Water Storage ; Time Variable Gravity ; Mass Balance ; Satellite Geodesy ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD ; Earth Observation Satellites 〉 NASA Earth System Science Pathfinder 〉 GRACE
    Language: English
    Type: Dataset , Dataset
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  • 82
    Publication Date: 2023-04-21
    Description: Abstract
    Description: This data publication encompasses a set of global tidal levels for individual epochs between 21 ka BP and present-day, the underlying global partial tides solutions (sea surface elevations and transports), and the global mean tidal dissipation as calculated from 8 partial tides. The data set was produced using the purely-hydrodynamical ocean tide model TiME, which was recently upgraded in the framework of the DFG-project Nerograv (https://www.lrg.tum.de/iapg/nerograv/) and which can be used for several applications: first, the reconstruction of indicative ranges for paleo sea levels markers, e.g. sea-level index points (SLIPs), second, to derive open boundary conditions for high-resolution regional paleo tide simulations, and third, to provide constraints for tidal deep ocean dissipation when running ocean general circulations models (OGCMs). The gridded information was transferred to a number of files in netcdf-format on a rotated-pole grid. The next section describes the creation of the data in more detail. Please also consider the data description for more details about the creation of this data set.
    Keywords: Tidal Dissipation ; Bessel Functions ; Data-unconstrained Ocean Tide Modelling ; Tidal Synthesis ; Linear Admittance Theory ; Analytical Modelling ; EARTH SCIENCE 〉 OCEANS 〉 COASTAL PROCESSES 〉 SEA LEVEL RISE ; EARTH SCIENCE 〉 OCEANS 〉 COASTAL PROCESSES 〉 SHORELINE DISPLACEMENT ; EARTH SCIENCE 〉 OCEANS 〉 COASTAL PROCESSES 〉 TIDAL HEIGHT ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL COMPONENTS ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL CURRENTS ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL HEIGHT ; EARTH SCIENCE 〉 OCEANS 〉 TIDES 〉 TIDAL RANGE ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 PALEOCLIMATE RECONSTRUCTIONS 〉 SEA LEVEL RECONSTRUCTION ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 COASTAL PROCESSES 〉 SEA LEVEL CHANGE
    Type: Dataset , Dataset
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  • 83
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    GFZ Data Services
    Publication Date: 2023-04-25
    Description: Abstract
    Description: The META-WT project was designed to perform a 4-weeks seismic experiment in Germany with a dense seismic array of ~400 three-component geophones that covered (1) a 2.5km x 2.5km wind farm area in Brandenburg, Germany, with almost 200 wind turbines (WTs) and a well-studied subsurface structure and (2) a 20-km long radial line from the center of the wind farm with one geophone every half-kilometer. The objective was to capture the spatio-temporal seismic wave-field signature of the wind farm from continuous recordings of ambient noise. Due to the dense interstation distance and proposed geometry the experiment allowed for analyzing both small-scale wave field characteristics at an unprecedented spatial resolution and the longer distance radiation pattern of the wind farm. Waveform data is available from the GEOFON data centre, under network code XF, and is embargoed until Jan 2025.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~400G
    Format: .mseed
    Format: XML
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  • 84
    Publication Date: 2023-04-26
    Description: Abstract
    Description: The Community Stress Drop Validation Study has been organized as a technical activity group (TAG) of SCEC (Southern California Earthquake Center) with the aim of investigating the source parameters of the 2019 Ridgecrest seismic sequence in California. Information about the stress drop TAG are available trough the benchmark web-page (https://www.scec.org/research/stress-drop-validation). Several groups applied different techniques to a shared data set with the objective of extracting source parameters (e.g. seismic moment and corner frequency) and in turn to estimate the stress drop. We applied a spectral decomposition approach known as generalized inversion technique (GIT) and the overall analyses are presented in a series of two articles (Bindi et al 2023a; Bindi et al 2023b). Results in the form of files, figures, and tables are disseminated through this archive.
    Keywords: 2019 Ridgecrest sequence ; source parameters ; spectral decomposition ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; geological process 〉 seismic activity 〉 earthquake
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  • 85
    Publication Date: 2023-04-26
    Description: Abstract
    Description: Organic matter (OM) is known to be an important reductant in sediment-hosted base metal deposits like the European Kupferschiefer. However, the precise nature of interactions between OM and hydrothermal fluids are still debated as well as how the interconnected reactions develop over geological timescales. This dataset provides for the first time bulk, compositional and stable isotope data of hydrocarbons, biomarkers and organonitrogen, -sulfur and-oxygen (NSO) compounds for the mineralized Kupferschiefer Spremberg-Graustein field in Eastern Germany based on samples from two drill cores. The study aims to help to better understand the role that organic matter plays during the mineralisation and formation of the sedimentary ore deposit within the Kupferschiefer with a focus on stable hydrogen isotope compositions and NSO compositional data to especially address the origin and to assess the oxidative nature of the brines that caused the mineralization in the Spremberg-Graustein field. The data publication includes bulk, compositional and stable isotope data on inorganic metals and organic matter. The data about metal contents were generated using ICP-MS while those on the organic matter were generated using Rock-Eval pyrolysis, a microscope, a Soxhlet apparatus, medium pressure liquid chromatography (MPLC), gas chromatography with flame ionization (GC-FID) and mass spectrometric detection (GC-MS), gas chromatography isotope ratio mass spectrometry (GC-IRMS) and ultrahigh resolution mass spectrometry (Fourier Transform ion cyclotron resonance mass spectrometry, FT-ICR-MS) with Electrospray ionization (ESI) and Atmospheric pressure photoionization (APPI). The full description of samples, methods and data is given in the following sections.
    Keywords: Kupferschiefer ; Permian ; Organic Matter ; NSO compounds ; hydrogen exchange ; metal porphyrins ; compound specific stable hydrogen isotopic composition ; FT-ICR-MS ; EARTH SCIENCE 〉 SOLID EARTH 〉 EARTH GASES/LIQUIDS 〉 PETROLEUM ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 METALS ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 SEDIMENTARY ROCKS
    Type: Dataset , Dataset
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  • 86
    Publication Date: 2023-04-27
    Description: Abstract
    Description: This dataset comprises 47 fluid samples from 11 geothermal sites (Germany, Austria, Iceland, Turkey, Netherlands, Belgium, French West Indies). The samples were collected within the REFLECT project (Redefining geothermal properties at extreme conditions to optimize future geothermal energy extraction). The focus with these analyses were on the organic compound composition of the fluids, since they are rarely included in the analyses of fluids taken from geothermal power plants. Understanding the organic compound composition of geothermal fluids might help to better understand chemical reactions within the fluids and might help to mitigate problems that arise with the operation of a geothermal power plant such as mineral precipitation (scaling) and corrosion of the casing and pipes.
    Description: Methods
    Description: The samples were taken by the onsite project partners and sent to GFZ for the analyses. Generally, the fluid samples were taken at the surface instalments and remained untreated after sampling (otherwise given as remark in the datasheet). Sampling bottles were rinsed and flushed with the fluids prior to filling them up. Sampling volumes ranged from 250-500 ml per sample.
    Keywords: Geothermal fluids ; Brine ; Dissolved organic matter ; Dissolved organic carbon ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 CHEMICAL CONCENTRATIONS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOTHERMAL DYNAMICS 〉 GEOTHERMAL ENERGY
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  • 87
    Publication Date: 2023-05-09
    Description: Abstract
    Description: This data publication contains a high resolution molecular dataset of a study aiming to trace variations in organic carbon sourcing along the Kali Gandaki River in Central Nepal. The data are on samples from different materials in the landscape (litter, soil, bedrock) and river sediments. On these samples we measured the extractable lipid fraction by measured by negative electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (ESI-FT-ICR-MS). The data was generated between 2015-05 and 2017-12. Please consult the associated data description and Menges et al. (2020) for more details.
    Keywords: organic carbon ; lipids ; EARTH SCIENCE 〉 LAND SURFACE 〉 EROSION/SEDIMENTATION 〉 SEDIMENT CHEMISTRY ; EARTH SCIENCE 〉 LAND SURFACE 〉 GEOMORPHOLOGY 〉 FLUVIAL LANDFORMS/PROCESSES ; In Situ/Laboratory Instruments 〉 Spectrometers/Radiometers 〉 MASS SPECTROMETERS
    Type: Dataset , Dataset
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  • 88
    Publication Date: 2023-05-11
    Description: Abstract
    Description: The Illgraben is a 10 km² steep side valley located in Switzerland. This active debris flow catchment supplies 5-15% of the total sediment load of the Rhône River upstream of Lake Geneva. The 30-80° steep catchment slopes host frequent rock falls and slides. From 2012 to 2014, a network of up to ten Nanometrics Trillium Compact 120s broadband seismometers, sampled by Digos DataCube³ext loggers at 200 Hz (and later by centaur), was deployed in and around the catchment to monitor distributed geomorphic activity. Waveform data is available from the GEOFON data centre, under network code 9J, and is fully open.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~100G
    Format: .mseed
    Format: XML
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  • 89
    Publication Date: 2023-05-12
    Description: Abstract
    Description: Sodankylä geophysical observatory (SGO) has operated in Sodankylä in northern Finland since 1913. SGO was originally founded by the Finnish Academy of Science and Letters. Now it takes care of national and international duties studying the space and geoenvironment as an independent research organisation in the University of Oulu. SGO performs long-term measurements, builds instruments, innovates and maintains domestic and international measurements, and performs research from these measurements. The seismic observations at SGO started in Sodankylä 1956. In 2005-2006 SGO seismic stations were updated to broadband instrumentation and connected to GEOFON data center. Today, the number of seismic stations has increased to 9. The stations have Streckeisen STS-2 or Nanometrics Trillium PA/PH broadband sensors. 3 of the stations are so called Posthole stations located in borehole 7-20 m below surface. The rest of the stations are located on the surface or in a more traditional type of vault. Data acquisition systems are either Earth Data PS6-24 digitisers and PC with Seiscomp or Nanometrics Centaurs. The continuous wave form data is collected at 100 Hz sampling frequency. The VH, LH and BH channel data is available from GEOFON data center and the 100Hz HH data from SGO by request. Further information about instrumentation can be found at the Institute’s web site (https://www.sgo.fi/). Waveform data are available from the GEOFON data centre, under network code FN, and arefully open.
    Keywords: geophysics ; seismology ; seismic noise ; earthquakes ; induced ; seismic hazard ; broad band ; velocity ; acceleration ; displacement ; Broadband seismic waveforms ; Seismic monitoring ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
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  • 90
    Publication Date: 2023-05-16
    Description: Abstract
    Description: The main component of this data publication is a dataset of predicted daily nutrient concentrations for NO3-N and TP for 150 monitoring stations along 60 German rivers (main rivers). The aim of this dataset is to fill the data gap of daily nutrient concentrations for a better understanding of nutrient transport from the rivers to the seas. So far, nutrient concentrations are sampled on a fortnightly basis, which can be insufficient for nutrient retention models working on a daily basis. With this method and available datasets, river basin managers have the opportunity to look at nutrient concentrations or load patterns on a finer resolution to adapt their management to improve water quality. The dataset was obtained by a random forest model (RF) based on measured NO3-N and TP concentrations between the years 2000 and 2019. The data was requested or where available downloaded from official websites of the Federal States or River Basins. Different variables for NO3-N and TP were finally considered in the models to produce the RF, like discharge, land use, day of the year.
    Description: TableOfContents
    Description: The following data is found in the data download zip file: Dataset as csv: Dataset of predicted daily nutrient concentrations for NO3-N and TP for 150 monitoring stations along 60 German rivers. Figures as pdf: Comparison of predicted values based on different distributions (mean and mode) for annual cycles of NO3-N and TP concentrations and loads for 150 locations along 60 rivers in Germany. Coding of monitoring stations as csv: The basic step for the analysis was finding pairs of gauges and water quality stations. These pairs were then coded and used in the model as ID. This coding file contains the names of monitoring stations and gauges for each ID as well as the number of NO3-N, TP concentrations, discharges and years applied. Variable importance as figure and explanation as csv: Several RF variants with different sets of variables were built. Starting with 11 variables and iteratively considering which were most important. Variables are explained in a csv and their importance for each variant is shown in the figure. Random Forests for TP and NO3-N as R.data: The best performing Random Forests for NO3-N (variant 7) and TP (variant 1) are stored as R.data files for further application.
    Keywords: daily nutrient concentration ; river ; Germany ; Random Forest ; Machine Learning ; prediction ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 SURFACE WATER 〉 RIVERS/STREAMS ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 SURFACE WATER 〉 SURFACE WATER CHEMISTRY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 WATER QUALITY/WATER CHEMISTRY 〉 NITROGEN COMPOUNDS ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 WATER QUALITY/WATER CHEMISTRY 〉 NUTRIENTS ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 WATER QUALITY/WATER CHEMISTRY 〉 PHOSPHOROUS COMPOUNDS ; environment 〉 natural environment 〉 aquatic environment ; environment 〉 physical environment 〉 abiotic environment ; In Situ/Laboratory Instruments 〉 Data Analysis 〉 Environmental Modeling 〉 Computer ; In Situ/Laboratory Instruments 〉 Gauges 〉 WATER LEVEL GAUGES ; In Situ/Laboratory Instruments 〉 Samplers 〉 Bottles/Flasks/Jars 〉 WATER BOTTLES ; In Situ/Laboratory Instruments 〉 Samplers 〉 Grabbers/Traps/Collectors 〉 GRAB SAMPLERS ; Models/Analyses 〉 MODELS ; The Present
    Type: Dataset , Dataset
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  • 91
    Publication Date: 2023-05-22
    Description: Abstract
    Description: “This ocean-bottom seismometer deployment is part of the SEAMSTRESS project examining tectonic stress effects on Arctic methane seepage. The project is led by PI Andreia Plaza-Faverola at the Centre for Arctic Gas Hydrates, University of Tromsö, Norway. A total of 10 ocean bottom seismometers (OBS) were deployed on Vestnesa Ridge, a sediment drift body just north Knipovich Ridge at its intersection with the Molloy Transform fault (cruise CAGE-20-5). The aim of the experiment was to look for stress release along faults that control seepage sites on Vestnesa Ridge. The network consisted of 8 Lobster type broadband OBS from the German Instrument Pool for Amphibian Seismology (DEPAS) and 2 3C geophones provided by the University of Tromsö. Instruments were free-fall deployed and spaced by about 10 km. They recorded continuously at 100 Hz for 11 months between August 2020 and July 2021.Short, intersecting refraction profiles were shot across all OBS stations, such that OBS positions at the seafloor could be determined within 10 m (cruise CAGE-21-3). Clock drift in this experiment was nonlinear and skew values were only obtained for 6 of the stations. Skew-corrected station VSN01 served as reference station to obtain the clock drift of all other stations using noise cross-correlation and subsequently correct also for the thus determined nonlinearity of time drift. Waveform data are available from the GEOFON data centre, under network code Y9 and are embargoed until July 2025.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; temporary local seismic network ; Ocean-bottom seismometer ; OBS ; Vestnesa Ridge ; passive seismology ; DEPAS ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
    Location Call Number Expected Availability
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  • 92
    Publication Date: 2023-05-22
    Description: Abstract
    Description: This ocean-bottom seismometer deployment is part of the LoCHnESs (Loki Castle Hydrothermal iN-situ Experiements and Surveys) project examining hydrothermal fluid circulation at Loki's Castle vent field. The project is led by PI Thibaut Barreyre at the Centre for Deep Sea Research, Department of Earth Science, University of Bergen, Norway. A total of 8 ocean bottom seismometers (OBS) were deployed near Loki's Castle vent field at the Mohns-Knipovich Ridge bend, Norwegian-Greenland Sea. The aim of the experiment was to monitor seismicity related to changes in the hydrothermal circulation system and to reveal interaction between an active detachment fault and the axial volcanic ridge hosting the vent site. The network consisted of 8 DEPAS Lobster type broadband OBS from the German Instrument Pool for Amphibian Seismology (DEPAS). Instruments were free-fall deployed and spaced by about 5-8 km. They recorded continuously at 100 Hz for 12 months between July 2019 and July 2020. Two instruments (LOK01 and LOK06) could only be deployed one month later and recorded at 250 Hz. OBS positions at the seafloor were determined by interpolation at 2/3 of the distance between the deployment and recovery position at the seafloor. Position accuracy is estimated to be about 100 m. Skew values were obtained for all stations and reached values of up to 24 s. Clock drift in this experiment was nonlinear. Skew-corrected station LOK02 served as reference station to obtain the clock drift of all other stations using noise cross-correlation and subsequently correct also for the thus determined nonlinearity of time drift. Waveform data are available from the GEOFON data centre, under network code 8M and are embargoed until July 2025.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; temporary local seismic network ; Ocean-bottom seismometer ; OBS ; Loki's Castle ; passive seismology ; DEPAS ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
    Location Call Number Expected Availability
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  • 93
    Publication Date: 2023-05-24
    Description: Abstract
    Description: This data set is a description of a novel analogue modelling method used to run lithospheric-scale tectonic models, and to uniquely monitor these models through X-Ray CT-scanning techniques at the Tectonic Modelling Lab of the University of Bern (Switzerland). It includes information on the model set-up and model materials, and includes a step-by-step description of the general modelling procedure. A first application of this novel procedure, for the simulation of lithospheric scale rifting processes can be found in Zwaan & Schreurs (2023a) in Tectonics, with supplementary data publicly available via GFZ Data Services (Zwaan & Schreurs 2023b). The results of this work prove the feasibility of the method, and opens the door to a broad variety of new tectonic modelling studies.
    Keywords: analogue modelling ; CT-scanning ; EPOS ; multi-scale laboratories ; analogue models of geologic processes ; analogue modelling results ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 PLATE TECTONICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 TECTONIC PROCESSES 〉 RIFTING
    Type: Other , Other
    Location Call Number Expected Availability
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  • 94
    Publication Date: 2023-05-26
    Description: Abstract
    Description: This data set was taken within the Perturbations of Earth Surface Processes by Large Earthquakes PRESSurE Project (https://www.gfz-potsdam.de/en/section/geomorphology/projects/pressure/) of the GFZ Potsdam. This project aims to better understand the role of earthquakes on earth surface processes. Strong earthquakes cause transient perturbations of the near Earth’s surface system. These include the widespread landsliding and subsequent mass movement and the loading of rivers with sediments. In addition, rock mass is shattered during the event, forming cracks that affect rock strength and hydrological conductivity. Often overlooked in the immediate aftermath of an earthquake, these perturbations can represent a major part of the overall disaster with an impact that can last for years before restoring to background conditions. Thus, the relaxation phase is part of the seismically induced change by an earthquake and needs to be monitored in order to understand the full impact of earthquakes on the Earth system. Early June 2015, shortly after the April 2015 Mw7.9 Gorkha earthquake, 6 automatic compact weather station were installed in the upper Bhotekoshi catchment covering an area ~50km2. The weather station network is centered around the Kahule Khola catchment, a small headwater catchment and is part of a wider data acquisition strategy including hydrological monitoring, seismometers, geophones and high resolution optical (RapidEye) as well as radar imagery (TanDEM TerraSAR-X). https://www.gfz-potsdam.de/sektion/geomorphologie/projekte/pressure/
    Keywords: rainfall ; Precipitation ; Nepal ; Himalayas ; Gorkha Earthquake ; perturbations ; Bhotekoshi River ; Weather station ; climate 〉 climate type 〉 continental climate 〉 mountain climate ; EARTH SCIENCE 〉 ATMOSPHERE 〉 PRECIPITATION 〉 PRECIPITATION AMOUNT ; EARTH SCIENCE 〉 ATMOSPHERE 〉 PRECIPITATION 〉 PRECIPITATION RATE ; EARTH SCIENCE 〉 ATMOSPHERE 〉 PRECIPITATION 〉 RAIN ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 LAND SURFACE 〉 SOILS 〉 SOIL EROSION ; EARTH SCIENCE 〉 LAND SURFACE 〉 TOPOGRAPHY 〉 TOPOGRAPHIC EFFECTS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 TECTONIC LANDFORMS 〉 MOUNTAINS ; In Situ Land-based Platforms 〉 WEATHER STATIONS/NETWORKS ; In Situ/Laboratory Instruments 〉 Gauges 〉 RAIN GAUGES ; land 〉 world 〉 Asia 〉 Southern Asia
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 95
    Publication Date: 2023-05-26
    Description: Abstract
    Description: This data set was taken within the Perturbations of Earth Surface Processes by Large Earthquakes PRESSurE Project (https://www.gfz-potsdam.de/en/section/geomorphology/projects/pressure/) of the GFZ Potsdam. This project aims to better understand the role of earthquakes on earth surface processes. Strong earthquakes cause transient perturbations of the near Earth’s surface system. These include the widespread landsliding and subsequent mass movement and the loading of rivers with sediments. In addition, rock mass is shattered during the event, forming cracks that affect rock strength and hydrological conductivity. Often overlooked in the immediate aftermath of an earthquake, these perturbations can represent a major part of the overall disaster with an impact that can last for years before restoring to background conditions. Thus, the relaxation phase is part of the seismically induced change by an earthquake and needs to be monitored in order to understand the full impact of earthquakes on the Earth system. Early June 2015, shortly after the April 2015 Mw7.9 Gorkha earthquake, 6 automatic compact weather station were installed in the upper Bhotekoshi catchment covering an area ~50km2. The weather station network is centered around the Kahule Khola catchment, a small headwater catchment and is part of a wider data acquisition strategy including hydrological monitoring, seismometers, geophones and high resolution optical (RapidEye) as well as radar imagery (TanDEM TerraSAR-X). https://www.gfz-potsdam.de/sektion/geomorphologie/projekte/pressure/
    Keywords: discharge ; river isotope chemistry ; Nepal ; Himalayas ; Gorkha Earthquake ; perturbations ; Bhotekoshi River ; PRESSurE ; Perturbations of Earth Surface Processes by Large Earthquakes ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 ATMOSPHERIC/OCEAN INDICATORS 〉 FRESH WATER RIVER DISCHARGE ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPE MEASUREMENTS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOCHEMISTRY 〉 GEOCHEMICAL PROPERTIES 〉 ISOTOPES ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 TECTONIC LANDFORMS 〉 MOUNTAINS ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 SURFACE WATER 〉 STAGE HEIGHT ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 SURFACE WATER 〉 SURFACE WATER CHEMISTRY ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 WATER QUALITY/WATER CHEMISTRY 〉 STABLE ISOTOPES ; hydrosphere 〉 hydrologic cycle 〉 water level ; In Situ/Laboratory Instruments 〉 Pressure/Height Meters 〉 PRESSURE GAUGES ; land 〉 world 〉 Asia 〉 Southern Asia
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 96
    Publication Date: 2023-05-25
    Description: Methods
    Description: Wood increment cores of 15 Quercus robur tree individuals were taken. Dendro-dated late wood from tree rings of 5 individuals was dissected (not pooled). After cellulose extraction and homogenization, 18O/16O-ratios of annually resolved samples were determined by Isotope Ratio Mass Spectrometry (IRMS). Time series of 18O/16O are given as delta-values versus VSMOW. Details can be found in the downloadable “data description” file.
    Description: Abstract
    Description: An annually resolved chronologies of oxygen isotopes from five living oak (Quercus robur) trees have been measured from tree ring cellulose covering up to the last 180 years (1836CE – 2020CE). This tree-ring stable isotope data set was established within the ‘Terrestrial Environmental Observatories’ (TERENO) of the Helmholtz Association. The site “Lake Tiefer See” is subject to the TERENO monitoring activities at the Northeast German Lowland Observatory coordinated by the GFZ German Research Centre for Geosciences in Potsdam. The data set comprises the δ18O records with respect to the international VSMOW standard. Lake Tiefer See (53°350 N, 12°320 E) is located 90 km NNW of Berlin in the morainic terrain of the NE-German Polish Basin. It is part of in the N–S trending Klocksin Lake Chain. The sampled trees are growing at the southern shore of the lake. Fifteen co-dominant Quercus robur tree individuals were cored at about 1.3m above ground from two opposite positions using an increment corer of 5 mm diameter (Suunto, Finland or Mora, Sweden).
    Keywords: tree rings ; latewood ; cellulose ; stable oxygen isotopes ; d18O ; 18O/16O ; time series ; chronology ; Lake Tiefer See ; Mecklenburg lake district ; Northeastern Germany ; oak ; Quercus robur ; TERENO ; TERENO Northeast ; TERENO Nordost ; TERrestrial ENvironmental Observatories ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS 〉 ISOTOPIC ANALYSIS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS 〉 ISOTOPIC ANALYSIS 〉 CARBON ISOTOPE ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 PALEOCLIMATE RECONSTRUCTIONS ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 TREE RINGS
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 97
    Publication Date: 2023-05-25
    Description: Methods
    Description: Wood increment cores of 15 Quercus robur tree individuals were taken. Dendro-dated late wood from tree rings of 5 individuals was dissected (not pooled). After cellulose extraction and homogenization, 13C/12C-ratios of annually resolved samples were determined by Isotope Ratio Mass Spectrometry (IRMS). Time series of 13C/12C are given as delta-values versus VPDB. Details can be found in the downloadable “data description” file.
    Description: Abstract
    Description: An annually resolved chronologies of carbon isotopes from five living oak (Quercus robur) trees have been measured from tree ring cellulose covering up to the last 180 years (1836CE – 2020CE). This tree-ring stable isotope data set was established within the ‘Terrestrial Environmental Observatories’ (TERENO) of the Helmholtz Association. The site “Lake Tiefer See” is subject to the TERENO monitoring activities at the Northeast German Lowland Observatory coordinated by the GFZ German Research Centre for Geosciences in Potsdam. The data set comprises the δ13C records with respect to the international VPDB standard. Lake Tiefer See (53°350 N, 12°320 E) is located 90 km NNW of Berlin in the morainic terrain of the NE-German Polish Basin. It is part of in the N–S trending Klocksin Lake Chain. The sampled trees are growing at the southern shore of the lake. Fifteen co-dominant Quercus robur tree individuals were cored at about 1.3m above ground from two opposite positions using an increment corer of 5 mm diameter (Suunto, Finland or Mora, Sweden).
    Keywords: Tree rings ; latewood ; cellulose ; stable carbon isotopes ; d13C ; 13C/12C ; time series ; chronology ; Lake Tiefer See ; Mecklenburg lake district ; Northeastern Germany ; oak ; Quercus robur ; TERENO ; TERENO Northeast ; TERENO Nordost ; TERrestrial ENvironmental Observatories ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS 〉 ISOTOPIC ANALYSIS ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 BIOLOGICAL RECORDS 〉 TREE RINGS 〉 ISOTOPIC ANALYSIS 〉 CARBON ISOTOPE ; EARTH SCIENCE 〉 CLIMATE INDICATORS 〉 PALEOCLIMATE INDICATORS 〉 PALEOCLIMATE RECONSTRUCTIONS ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 TREE RINGS
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 98
    Publication Date: 2023-06-02
    Description: Abstract
    Description: This folder contains the scripts, input and output files required to calculate the inter-scheme conversion matrices for building types and the implicit damage states of their respective fragility models for two selected vulnerability schemes: one for earthquakes and the other for tsunamis. They were used in previous studies to characterize the residential building stock of Lima. The outcomes generated in this data repository are valuable inputs to then calculate the disaggregated and cumulative damage and losses expected for cascading hazard scenarios.
    Description: Other
    Description: In recent decades, the risk to society due to natural hazards has increased globally. To counteract this trend, effective risk management is necessary, for which reliable information is essential. Most existing natural hazard and risk information systems address only single components of a complex risk assessment chain, such as, for instance, focusing on specific hazards or simple loss measures. Complex interactions, such as cascading effects, are typically not considered, as well as many of the underlying sources of uncertainty. This can lead to inadequate or even miss-leading risk management strategies, thus hindering efficient prevention and mitigation measures, and ultimately undermining the resilience of societies. Therefore, experts from different disciplines work together in the joint project RIESGOS 2.0 (Scenario-based multi-risk assessment in the Andes region) and develop innovative scientific methods for the evaluation of complex multi-risk situations with the aim to transfer the results as web services into a demonstrator for a multi-risk information system.
    Keywords: machine learning ; vulnerability ; multi-hazard ; earthquake fragility ; tsunami fragility ; cumulative damage ; Bayesian approach ; RIESGOS ; Scenario-based multi-risk assessment in the Andes region ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 TSUNAMIS
    Type: Dataset , Dataset
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  • 99
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    Unknown
    GFZ Data Services
    Publication Date: 2023-06-02
    Description: Abstract
    Description: Within the Inter-Wind project we study wind turbine (WT) emissions with ground motion and acoustic measurements which are accompanied by the acquisition of meteorological parameters as well as psychological surveys of residents living in the vicinity of the wind farms. Measurements are conducted on the Swabian Alb in Southern Germany at wind farms Tegelberg and Lauterstein in multiple interdisciplinary campaigns. Here we focus on measurements with line and ring layouts which are directed at improving the prediction of ground-motion emissions of WTs. This dataset contains recorder log files. Seismic data is stored at GEOFON, network 4C (2020 - 2024, Ritter and Gaßner 2022).
    Keywords: Wind turbine signals ; line measurement ; PASSIVE_SEISMIC 〉 NETWORK ; SENSOR 〉 SEISMOMETER ; SENSOR 〉 GEOPHONE ; SENSOR 〉 3-C ; LAND ; AUXILIARY_DATA
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 100
    Publication Date: 2023-06-02
    Description: Abstract
    Description: This data repository contains a brief description of the building classification scheme for physical vulnerability to tsunamis and corresponding fragility functions originally proposed by Medina, 2019. These fragility functions are used as input to construct their associated state-dependent fragility functions using scaling factors, which were obtained as ad-hoc calibration parameters. A Python script to produce a file with such a model is provided along with the needed inputs and resulting output files.
    Description: Other
    Description: In recent decades, the risk to society due to natural hazards has increased globally. To counteract this trend, effective risk management is necessary, for which reliable information is essential. Most existing natural hazard and risk information systems address only single components of a complex risk assessment chain, such as, for instance, focusing on specific hazards or simple loss measures. Complex interactions, such as cascading effects, are typically not considered, as well as many of the underlying sources of uncertainty. This can lead to inadequate or even miss-leading risk management strategies, thus hindering efficient prevention and mitigation measures, and ultimately undermining the resilience of societies. Therefore, experts from different disciplines work together in the joint project RIESGOS 2.0 (Scenario-based multi-risk assessment in the Andes region) and develop innovative scientific methods for the evaluation of complex multi-risk situations with the aim to transfer the results as web services into a demonstrator for a multi-risk information system.
    Keywords: fragility function ; tsunami vulnerability ; multi-hazard ; attributes ; RIESGOS ; Scenario-based multi-risk assessment in the Andes region ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 EARTHQUAKES ; EARTH SCIENCE 〉 HUMAN DIMENSIONS 〉 NATURAL HAZARDS 〉 TSUNAMIS
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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