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  • Data  (12,405)
  • 2020-2020
  • 2015-2019  (12,405)
  • 1945-1949
  • 2016  (12,405)
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  • 2020-2020
  • 2015-2019  (12,405)
  • 1945-1949
Year
  • 1
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    Supplement to: The New World Atlas of Artificial Night Sky Brightness (2016)
    GFZ Data Services
    Details
    Publication Date: 2021-10-05
    Description: Abstract
    Description: These are maps of artificial night sky radiance that were produced by the Light Pollution Science and Technology Institute (ISTIL), and described in the paper "The New World Atlas of Artificial Night Sky Brightness" (Falchi et al. 2016).The data are stored in a 2.9 Gb geotiff file, on a 30 arcsecond grid. The map reports simulated zenith radiance data in [mcd/m^2]. The map is based on data from the VIIRS Day Night Band (DNB, MIller et al. 2013), which has been propagated through the atmosphere using the radiative transfer code reported in (Cinzano and Falchi, 2012). The upward emission function and the radiance calibration were obtained using data from Sky Quality Meters (including data from Duriscoe et al. 2007; Falchi 2010; Kyba et al 2013, 2015 and Zamorano et al. 2016).Note that the maps report artificial light only! The zenith radiance from natural sources such as stars and the Milky Way are not included, and must be added in order to match the data that would be obtained from an actual outdoor measurement.A kmz file for quick view of the data is also provided. Access to the FTP site to download the data can be requested via the data request form on the landing page.Version History:13 November 2019: change of the licence to CC BY NC 4.0 (after end of embargo period).
    Description: Other
    Description: Artificial lights raise the night sky luminance, creating the most visible effect of light pollution, artificial sky glow. Despite the increasing interest among scientists in fields such as ecology, astronomy, healthcare, land use planning, light pollution lacks a current quantification of its magnitude on a global scale. To overcome this, here we present the World atlas of the artificial sky luminance, computed with our light pollution propagation software using new high resolution satellite data and new precision sky brightness measurements. This atlas shows that more than 80% of the World and more than 99% of the U.S.A. and Europe populations live under light polluted skies. The Milky Way is hidden for more than one third of humanity, including 60% of Europeans and nearly 80% of North Americans. Moreover, 23% of World's lands between 75°N and 60°S, 88% of Europe and almost half of U.S.A. experience light polluted nights.
    Keywords: artificial light ; ALAN ; skyglow ; light pollution ; atlas ; night ; radiative transfer ; Suomi NPP ; Sky Quality Meter ; EARTH SCIENCE SERVICES 〉 DATA ANALYSIS AND VISUALIZATION 〉 VISUALIZATION/IMAGE PROCESSING
    Language: English
    Type: Dataset , Dataset
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  • 2
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    Preface (2016)
    Geographisches Institut der Universität zu Köln - Kölner Geographische Arbeiten
    Details
    Publication Date: 2022-01-12
    Description: Abstract
    Description: The 2nd Data Management Workshop was held at the University of Cologne in November 2014. It was organized within the research data management activities of two large interdisciplinary research projects both funded by the German Research Foundation (DFG). Both projects actively supported the workshop. The Collaborative Research Centre/Transregio 32 ‘Patterns in Soil-Vegetation-Atmosphere Systems: Monitoring, Modelling and Data Assimilation’ involves scientist from the fields of meteorology, hydrology, geography, geophysics, soil sciences and mathematics. The CRC806 ‘Our Way to Europe: Culture-Environment Interaction and Human Mobility in the Late Quaternary’ integrates scientists from the disciplines of prehistoric archaeology, geology, geography, geophysics and soil sciences. Organizing research data management of such diverse disciplines which are distributed over several universities and research centers faces several problems and challenges. Consequently, the main focus of the 2nd Data Management Workshop was to discuss solutions and approaches for interdisciplinary and disciplinary data management with other colleagues and experts of the field. The publication of the Special Issue on ‘Research Data Management’ of the ISPRS International Journal of Geo-Information (ISSN 2220-9964) emerged in the context of this workshop.
    Description: SeriesInformation
    Description: Proceedings of the 2nd Data Management Workshop, 28.-29.11.2014, University of Cologne, Germany, Kölner Geographische Arbeiten, 96, pp. III-IV
    Keywords: Data Management ; Research Data
    Language: English
    Type: Text , Workshop paper
    Format: 2 Pages
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  • 3
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    Research Data Management within the E-Science Strategy in Baden-Württemberg - Preliminary Results of Project bwFDM-Communities (2016)
    Geographisches Institut der Universität zu Köln - Kölner Geographische Arbeiten
    Details
    Publication Date: 2022-01-12
    Description: Abstract
    Description: The federal state of Baden-Württemberg wants to offer scientists the best conditions for research. Against the backdrop of the ever-increasing importance of data and information the bwFDM-Communities project is tasked to develop recommendations that shall enable scientists in our federal state to process and use data without barriers. In order to achieve this objective, we engage an active dialogue with all university research groups in Baden-Württemberg (~3000). Next to identifying and advertising best-practice solutions, this project is supposed to gather information on how federal IT support needs to be expanded in order to meet the increasing demands of future research. As this is an ongoing project there may be further results in time, but some early conclusions can be drawn: Scientists want clear-cut requirements and responsibilities for data management and are willing to share their data if there is a proper appreciation model for data publication. Additionally, a lot of scientists complain about too strict law regulations regarding copyright and need better information about available RDM support, partners and opportunities. Final conclusions and recommendations can only be given in the further course of the project, but we are confident that our final recommendations will help the scientists in Baden-Württemberg.
    Description: SeriesInformation
    Description: Proceedings of the 2nd Data Management Workshop, 28.-29.11.2014, University of Cologne, Germany, Kölner Geographische Arbeiten, 96, pp. 1-6
    Keywords: Data Management ; Research Data
    Language: English
    Type: Text , Workshop paper
    Format: 6 Pages
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  • 4
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    The TR32DB: A Research Data Management System for the CRC/Transregio 32 ‘Patterns in Soil-Vegetation-Atmosphere Systems’ (2016)
    Geographisches Institut der Universität zu Köln - Kölner Geographische Arbeiten
    Details
    Publication Date: 2022-01-12
    Description: Abstract
    Description: This paper introduces the CRC/TR32 database (TR32DB), a research data management system developed within the multidisciplinary research project Collaborative Research Centre/Transregio 32 (CRC/TR32) funded by the German Research Foundation (DFG). The aim of the TR32DB is to support collative research within the whole project by providing data storage, backup, archive, documentation, publication and also sharing services. The entire system is self-developed according to the requirements of the funding agency, the user and project demands, as well as according to recent principles and standards. The TR32DB system architecture is basically a combination of data storage (file management), database and web-interface. In addition, the TR32DB Metadata Schema was designed and implemented to describe all project data with accurate metadata. A user-friendly multi-level approach was chosen to cover the requirements of all data stored in the TR32DB with appropriate metadata.
    Description: SeriesInformation
    Description: Proceedings of the 2nd Data Management Workshop, 28.-29.11.2014, University of Cologne, Germany, Kölner Geographische Arbeiten, 96, pp. 7-15
    Keywords: Data Management ; Metadata ; Research Data
    Language: English
    Type: Text , Workshop paper
    Format: 9 Pages
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  • 5
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    GFZ VER11 SLCCI precise orbits of altimetry satellites ERS-1, ERS-2, Envisat, TOPEX/Poseidon, Jason-1 and Jason-2 in the ITRF2008 (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-01-17
    Description: Abstract
    Description: The data set provides GFZ VER11 orbits of altimetry satellitesERS-1 (August 1, 1991 - July 5, 1996),ERS-2 (May 13, 1995 - February 27, 2006),Envisat (April 12, 2002 - April 8, 2012),Jason-1 (January 13, 2002 - July 5, 2013) andJason-2 (July 5, 2008 - April 5, 2015)TOPEX/Poseidon (September 23, 1992 - October 8, 2005),derived at the time spans given at Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences within the Sea Level phase 2 project of the European Space Agency (ESA) Climate Change Initiative using "Earth Parameter and Orbit System - Orbit Computation (EPOS-OC)" software and the Altimeter Database and processing System (ADS, http://adsc.gfz-potsdam.de/ads/) developed at GFZ. The orbits were computed in the same (ITRF2008) terrestrial reference frame for all satellites using common, most precise models and standards available and described below.The ERS-1 orbit is computed using satellite laser ranging (SLR) and altimeter crossover data, while the ERS-2 orbit is derived using additionally Precise Range And Range-rate Equipment (PRARE) measurements. The Envisat, TOPEX/Poseidon, Jason-1 and Jason-2 orbits are based on Doppler Orbitography and Radiopositioning Integrated by Satellite (DORIS) and SLR observations.The orbit files are available in the Extended Standard Product 3 Orbit Format (SP3-c, ftp://igscb.jpl.nasa.gov/igscb/data/format/sp3c.txt) Files are gzip-compressed. File names are given as sate_YYYYMMDD_SP3C.gz, where "sate" is the abbreviation (ENVI, ERS1, ERS2, JAS1, JAS2, TOPX) of the satellite name, YYYY stands for 4-digit year, MM stands for month and DD stands for day of the beginning of the file.More details on these orbits are provided in Rudenko et al. (2017)
    Keywords: Jason-1 ; Jason-2 ; ERS-1 ; ERS-2 ; Envisat ; ESA CCI Sea Level ; Altimetry satellite ; Low Earth Orbit satellites ; sea level ; TOPEX/POSEIDON ; ITRF2008 ; Earth Remote Sensing Instruments 〉 Active Remote Sensing 〉 Altimeters 〉 Radar Altimeters ; equipment 〉 artificial satellite 〉 observation satellite ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 SATELLITE ORBITS/REVOLUTION 〉 ORBITAL POSITION ; EARTH SCIENCE 〉 OCEANS 〉 SEA SURFACE TOPOGRAPHY 〉 SEA SURFACE HEIGHT
    Language: English
    Type: Dataset
    Format: 6 Files
    Format: application/octet-stream
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  • 6
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    Neusling (Landau a.d. Isar) 2012 - A Multitemporal and Multisensoral Agricultural EnMAP Preparatory Flight Campaign (Datasets) (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-03-11
    Description: Abstract
    Description: This data collection contains a multitemporal series of six airborne hyperspectral image mosaics acquired during the growing season of 2012 over the Neusling test area near Landau a.d. Isar in Southern Germany. The airborne hyperspectral data is complemented by accompanying in-situ data acquired parallel to the overflights. The dataset is composed of a) four airborne hyperspectral image mosaics acquired during overflights on April 28th 2012, May 25th 2012, June 16th 2012 and September 8th 2012 with the AVIS-3 imaging spectrometer. The AVIS data consists of 197 spectral bands, ranging from VIS to SWIR (477 - 1704 nm); b) two airborne hyperspectral image mosaics acquired during overflights, which were conducted by the DLR user service OpAiRS (www.dlr.de/opairs) on May 8th 2012 and August 14th 2012 with a HySpex imaging spectrometer. The HySpex data consists of 332 spectral bands, ranging from VIS to SWIR (417 - 2496 nm); c) spatially comprehensive land use/land cover maps generated from in-situ observations for two time-windows during the growing season of 2012 (May and August); d) Flight-parallel in-situ point-measurements consisting of: i) non-destructively measured leaf area index of winter wheat, winter barley, sugar beet, maize and rapeseed (561 measurements incl. standard deviations), ii) SPAD chlorophyll measurements (522 measurements incl. standard deviations), iii) 557 soil moisture measurements incl. standard deviations iv) 539 phenological observations v) 499 measurements of canopy height incl. standard deviations and vi) 38 measurements of plant density. The dataset was collected in order to cover the seasonal dynamics in the development of agricultural crops in Southern Germany.Version History: Correct Acquisition date of the second HySpex flight was August 14th 2012, not August 12th 2012.
    Description: Other
    Description: The Environmental Mapping and Analysis Program (EnMAP) is a German hyperspectral satellite mission that aims at monitoring and characterizing the Earth’s environment on a global scale. EnMAP serves to measure and model key dynamic processes of the Earth’s ecosystems by extracting geochemical, biochemical and biophysical parameters, which provide information on the status and evolution of various terrestrial and aquatic ecosystems. In the frame of the EnMAP preparatory phase, pre-flight campaigns including airborne and in-situ measurements in different environments and for several application fields are being conducted. The main purpose of these campaigns is to support the development of scientific applications for EnMAP. In addition, the acquired data are input in the EnMAP end-to-end simulation tool (EeteS) and are employed to test data pre-processing and calibration-validation methods. The campaign data are made freely available to the scientific community under a Creative Commons Attribution-ShareAlike 4.0 International License. An overview of all available data is provided in in the EnMAP Flight Campaigns Metadata Portal http://www.enmap.org/?q=flights.
    Keywords: Hyperspectral Imagery ; Field Spectroscopy ; Agriculture ; LAI
    Language: English
    Type: Dataset , Dataset
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  • 7
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    Climatologies at high resolution for the earth's land surface areas (Version 1.0) (2016)
    WDCC
    Details
    Publication Date: 2022-04-25
    Description: CHELSA_v1.0 (http://chelsa-climate.org/) is a high resolution (30 arc sec, ~1 km) climate data set for the earth land surface areas. Version 1.0 is a first release. It includes monthly and annual mean temperature and precipitation patterns for the time period 1979-2013. CHELSA_v1 is based on a quasi-mechanistical statistical downscaling of the ERA interim global circulation model (http://www.ecmwf.int/en/research/climate-reanalysis/era-interim) with a GPCC (https://www.dwd.de/EN/ourservices/gpcc/gpcc.html) and GHCN (https://www.ncdc.noaa.gov/ghcnm/) bias correction. Specifications: High resolution (30 arcsec, ~1 km) Precipitation & Temperature Monthly coverage 1979 - 2013 Incorporation of topoclimate (e.g. orographic rainfall & wind fields). Downscaled ERA-interim model. Allows calculation of derived parameters based on monthly values such as length of dry periods etc.
    Type: experiment
    Format: GeoTIFF
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  • 8
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    Climatologies at high resolution for the earth's land surface areas (Version 1.1) (2016)
    WDCC
    Details
    Publication Date: 2022-04-25
    Description: CHELSA_v1.1 (http://chelsa-climate.org/) is a high resolution (30 arc sec, ~1 km) climate data set for the earth land surface areas. It includes monthly and annual mean temperature and precipitation patterns as well as derived bioclimatic and interannual parameters for the time period 1979-2013. CHELSA_v1.1 is based on a quasi-mechanistical statistical downscaling of the ERA interim global circulation model (http://www.ecmwf.int/en/research/climate-reanalysis/era-interim) with a GPCC (https://www.dwd.de/EN/ourservices/gpcc/gpcc.html) and GHCN (https://www.ncdc.noaa.gov/ghcnm/) bias correction.
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  • 9
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    coastDat-2 WAM-North_Sea (2016)
    WDCC
    Details
    Publication Date: 2022-04-25
    Description: This is a North Sea wave hindcast for the period 1949-2014. The simulation has been performed with the wave model WAM Version 4.5.4. The model domain covers the area from 51N to 59N and 4.75W to 13E, with a spatial resolution of 0.05 degree latitude x 0.075 degree longitude (approx. 3 by 3 nautical miles). Integrated parameter derived from 2D spectra are available every hour. Atmospheric forcing was obtained from an atmospheric hindcast with COSMO-CLM (doi:10.1594/WDCC/coastDat-2_COSMO-CLM) driven by the NCEP/NCAR Reanalysis 1 data set. Lateral boundary conditions were obtained from corresponding coarse grid hindcast covering most of the Northeast Atlantic driven by the same atmospheric forcing.
    Type: experiment
    Format: NetCDF
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  • 10
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    eVolv2k_v1: an ice-core based volcanic stratospheric sulfur injection database (2016)
    WDCC
    Details
    Publication Date: 2022-04-25
    Description: This dataset contains ice core-based estimates of volcanic stratospheric sulfur injections covering the years 500 BCE to 1900 CE. Ice core-derived volcanic sulfate deposition composites for Antarctica (Sigl et al., 2014) and Greenland (Sigl et al., 2015) are scaled to volcanic stratospheric sulfur injection based on a method similar to that of Gao et al., (2007). Sigl, M., Winstrup, M., McConnell, J. R., Welten, K. C., Plunkett, G., Ludlow, F., Büntgen, U., Caffee, M., Chellman, N., Dahl-Jensen, D., Fischer, H., Kipfstuhl, S., Kostick, C., Maselli, O. J., Mekhaldi, F., Mulvaney, R., Muscheler, R., Pasteris, D. R., Pilcher, J. R., Salzer, M., Schüpbach, S., Steffensen, J. P., Vinther, B. M. and Woodruff, T. E.: Timing and climate forcing of volcanic eruptions for the past 2,500 years, Nature, 523, 543-549, doi:10.1038/nature14565, 2015. Sigl, M., McConnell, J. R., Toohey, M., Curran, M., Das, S. B., Edwards, R., Isaksson, E., Kawamura, K., Kipfstuhl, S., Krüger, K., Layman, L., Maselli, O. J., Motizuki, Y., Motoyama, H., Pasteris, D. R. and Severi, M.: Insights from Antarctica on volcanic forcing during the Common Era, Nat. Clim. Chang., 4, 693-697, doi:10.1038/nclimate2293, 2014. Gao, C., Oman, L., Robock, A. and Stenchikov, G. L.: Atmospheric volcanic loading derived from bipolar ice cores: Accounting for the spatial distribution of volcanic deposition, J. Geophys. Res., 112(D9), doi:10.1029/2006JD007461, 2007.
    Type: experiment
    Format: NetCDF
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  • 11
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    Stress Map Germany 2016 (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-07-08
    Description: Abstract
    Description: The stress map of Germany shows the orientation of the current maximum horizontal stress (SHmax) in the earth's crust. Assuming that the vertical stress (SV) is a principal stress, SHmax defines the orientation of the 3D stress tensor; the minimum horizontal stress Shmin is than perpendicular to SHmax. In the stress map the SHmax orientations are represented as lines of different lengths. The length of the line is a measure of the quality of data and the symbol shows the stress indicator and the color the stress regime. Data with E-Quality are shown without additional information as dots on the map. The stress data are freely available and part of the World Stress Map (WSM) project. For more information about the data and criteria of data analysis and quality mapping are plotted along the WSM website at http://www.world-stress-map.org.The German version of the World Stress Map Germany is available via http://doi.org/10.5880/WSM.Germany2016.
    Description: Other
    Description: The World Stress Map (WSM) is a global compilation of information on the crustal present-day stress field. It is a collaborative project between academia and industry that aims to characterize the stress pattern and to understand the stress sources. It commenced in 1986 as a project of the International Lithosphere Program under the leadership of Mary-Lou Zoback. From 1995-2008 it was a project of the Heidelberg Academy of Sciences and Humanities headed first by Karl Fuchs and then by Friedemann Wenzel. Since 2009 the WSM is maintained at the GFZ German Research Centre for Geosciences and since 2012 the WSM is a member of the ICSU World Data System. All stress information is analysed and compiled in a standardized format and quality-ranked for reliability and comparability on a global scale.
    Keywords: crustal stress ; in situ stress ; tectonic stress ; crustal stress pattern ; World Stress Map
    Type: Dataset
    Format: 9901520 Bytes
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  • 12
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    Stress Map Iceland 2016 (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-07-08
    Description: Abstract
    Description: The stress map of Iceland shows the orientation of the current maximum horizontal stress (SHmax) in the earth's crust. Assuming that the vertical stress (SV) is a principal stress, SHmax defines the orientation of the 3D stress tensor; the minimum horizontal stress Shmin is than perpendicular to SHmax. In the stress map the SHmax orientations are represented as lines of different lengths. The length of the line is a measure of the quality of data and the symbol shows the stress indicator and the color the stress regime. Data with E-Quality are shown without additional information as dots on the map. The stress data are freely available and part of the World Stress Map (WSM) project. For more information about the data and criteria of data analysis and quality mapping are plotted along the WSM website at http://www.world-stress-map.org.
    Description: Other
    Description: The World Stress Map (WSM) is a global compilation of information on the crustal present-day stress field. It is a collaborative project between academia and industry that aims to characterize the stress pattern and to understand the stress sources. It commenced in 1986 as a project of the International Lithosphere Program under the leadership of Mary-Lou Zoback. From 1995-2008 it was a project of the Heidelberg Academy of Sciences and Humanities headed first by Karl Fuchs and then by Friedemann Wenzel. Since 2009 the WSM is maintained at the GFZ German Research Centre for Geosciences and since 2012 the WSM is a member of the ICSU World Data System. All stress information is analysed and compiled in a standardized format and quality-ranked for reliability and comparability on a global scale.
    Keywords: crustal stress ; in situ stress ; tectonic stress ; crustal stress pattern ; mid ocean ridge
    Language: English
    Type: Dataset , Dataset
    Format: 11932019 Bytes
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  • 13
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    Stress Map of the Mediterranean and Central Europe 2016 (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-07-08
    Description: Abstract
    Description: The Stress Map of the Mediterranean and Central Europe 2016 displays 5011 A-C quality stress data records of the upper 40 km of the Earth’s crust from the WSM database release 2016 (Heidbach et al, 2016, http://doi.org/10.5880/WSM.2016.001). Focal mechanism solutions determined as being potentially unreliable (labelled as Possible Plate Boundary Events in the database) are not displayed. Further detailed information on the WSM quality ranking scheme, guidelines for the various stress indicators, and software for stress map generation and the stress pattern analysis is available at www.world-stress-map.org.
    Description: Other
    Description: The World Stress Map (WSM) is a global compilation of information on the crustal present-day stress field. It is a collaborative project between academia and industry that aims to characterize the stress pattern and to understand the stress sources. It commenced in 1986 as a project of the International Lithosphere Program under the leadership of Mary-Lou Zoback. From 1995-2008 it was a project of the Heidelberg Academy of Sciences and Humanities headed first by Karl Fuchs and then by Friedemann Wenzel. Since 2009 the WSM is maintained at the GFZ German Research Centre for Geosciences and since 2012 the WSM is a member of the ICSU World Data System. All stress information is analysed and compiled in a standardized format and quality-ranked for reliability and comparability on a global scale.
    Keywords: crustal stress ; in situ stress ; tectonic stress ; crustal stress pattern ; tectonics ; geophysics ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 STRESS ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 PLATE TECTONICS 〉 LITHOSPHERIC PLATE MOTION 〉 PLATE MOTION DIRECTION ; EARTH SCIENCE SERVICES 〉 DATA MANAGEMENT/DATA HANDLING 〉 DATA SEARCH AND RETRIEVAL
    Type: Dataset
    Format: 13765676 Bytes
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  • 14
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    Dead Sea Seismic Array, Jordan for DESERVE Project (Feb. 2014 - Feb. 2015) - Datasets (2016)
    Deutsches GeoForschungsZentrum GFZ
    Details
    Publication Date: 2022-11-29
    Description: Abstract
    Description: A temporary seismic array was installed in combination with a meteorological station in the Dead Sea valley, Jordan. Within the scope of the HGF virtual institute DESERVE we operated 15 temporary seismic stations between February 2014 and February 2015 together with a nearby meteorological station close to the east coast of the Dead Sea. The main aim was to acquire data to study the influence of wind on seismic records and retrieve related meteorological parameters. The study area is scarcely populated and has ideal meteorological conditions to study periodically occurring winds.
    Keywords: Seismology ; Array ; Noise ; Wind
    Language: English
    Type: Dataset , controlled source data
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  • 15
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    EnGeoMAP Test Data: Simulated EnMAP Satellite Data for Mountain Pass, USA and Rodalquilar, Spain (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-12-02
    Description: Abstract
    Description: This data pubilcation includes EnMAP-like imaging spectroscopy data files to be used for mineral mapping with the EnMAP BOX software. It is simulated EnMAP satellite data, which is based on hyperspectral flight campaign data with the AVIRIS-NG and HyMap sensors. In preparation of the EnMAP satellite mission, an EnMAP BOX software package provides tools for visualization and scientific analysis of the data. Among many applications, the EnMAP BOX contains geological mapping tools (EnGeoMAP). Here we apply these tools to several representative test cases (Boesche, 2015; Boesche et al. 2016; Mielke et al., 2016). The test data comprise two study sites. The first scene covers the Mountain Pass open pit mine - a carbonatite deposit in California, USA. It contains calcitic rock units and rare earth element (REE) bearing minerals of the bastnaesite group, also called fluorocarbonates (Olson et al., 1954). The REE concentrations at mountain pass are 9.2% on average, among the highest in the world (Brüning and Böhmer, 2011). The high concentration and the open pit activities make Mountain Pass an ideal test site to investigate the rare earth element distribution in the surface layer. The airborne image data were collected in 2014 by Jet Propulsion Laboratory (JPL), USA, with the AVIRIS-NG sensor and form the basis for EnMAP simulations (Segl et al., 2012; Thompson et al., 2015). The second HyMap spectral image data covers part of the Miocene Cabo de Gata Nίjar volcanic field, in southeast Spain. It comprises a subset of (Chabrillat et al., 2016) covering the Rodalquilar and Lomilla Calderas, which host the economically relevant gold-silver, lead-zinc-silver-gold and alunite deposits. It is a hydrothermal alteration complex, representing the silicic alteration, the advanced argillic alteration zone, which grades into the argillic and propylitic zone (Arribas et al., 1995, 1989). The image data are part of the Cabo de Gata Nίjar HyMap imagery which was collected during the DLR HyEurope airborne campaign 2005 in the frame of the GFZ land degradation program (Chabrillat et al., 2016, 2005). We use these datasets to simulate EnMAP-like images for classification and mapping using spectroscopic remote sensing techniques in the EnGeoMAP tools. The EnMAP end-to-end Simulation (EeteS) tool produced simulated EnMAP like data with a spatial sampling distance of 30 x 30 m and 242 spectral bands (Guanter et al., 2015; Segl et al., 2012). File format for both sites: Band Sequential Image Files (*.bsq) and file header (*.hdr). The full description of the datasets is given in the associated data report by Boesche et al. (2016).
    Description: Other
    Description: The Environmental Mapping and Analysis Program (EnMAP) is a German hyperspectral satellite mission that aims at monitoring and characterizing the Earth’s environment on a global scale. EnMAP serves to measure and model key dynamic processes of the Earth’s ecosystems by extracting geochemical, biochemical and biophysical parameters, which provide information on the status and evolution of various terrestrial and aquatic ecosystems. In the frame of the EnMAP preparatory phase, pre-flight campaigns including airborne and in-situ measurements in different environments and for several application fields are being conducted. The main purpose of these campaigns is to support the development of scientific applications for EnMAP. In addition, the acquired data are input in the EnMAP end-to-end simulation tool (EeteS) and are employed to test data pre-processing and calibration-validation methods. The campaign data are made freely available to the scientific community under a Creative Commons Attribution-ShareAlike 4.0 International License. An overview of all available data is provided in in the EnMAP Flight Campaigns Metadata Portal http://www.enmap.org/?q=flights.
    Keywords: Imaging spectroscopy ; Mineral Mapping ; Rare Earth Elements ; EnMAP ; EnGeoMAP ; Simulated Data ; Rodalquilar ; Mountain Pass ; Hyperspectral Imagery ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 MINERALS 〉 MINERAL PHYSICAL/OPTICAL PROPERTIES 〉 REFLECTION ; mineral resource ; satellite image
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  • 16
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    The Slovenian hybrid quasi-geoid: SLO-VRP2016/Koper (2016)
    GFZ Data Services
    Details
    Publication Date: 2022-12-06
    Description: Abstract
    Description: The SLO-VRP2016/Koper quasi-geoid model is the latest height reference surface for Slovenia, referred to the GRS80 ellipsoid. The acronym means SLOvenska Višinska Referenčna Ploskev iz leta 2016, datum Koper (translated in English, Slovenian Height Reference Surface from the year 2016, datum Koper). It was computed by the Surveying and Mapping Authority of the Republic of Slovenia, in cooperation with the Norwegian Mapping Authority (Kartverket). The model is based on a set of old terrestrial gravity data (origin from Yugoslavia, from 1956-75), a set of new Slovenian gravity data (along levelling lines and regional gravimetric survey, from 2000 to 2015) and sets from neighboring countries (Italy, Austria, Hungary and Croatia), altogether 16.400 points in the mean-tide system. Stokes/Molodensky equations and the Fast Fourier transform technique have been applied with use of global geopotential model EGM2008. The computed quasi-geoid surface was adapted (fitted) to 66 high quality GNSS/levelling points, which were fairly distributed throughout the territory of Slovenia. Therefore, the resulting quasi geoid model can be used to perform the conversion between ellipsoidal heights (Slovenian realization of ETRS89 - D96, GRS80 ellipsoid) and normal heights (Slovenian Height System 2010 - SVS2010 with Koper tide gauge). The SLO_VRP2016/Koper model is given in the form of a regular grid, with resolution of 30” × 45”, within the limits of 13° 〈 λ 〈 17° (east of Greenwich) and 45° 〈 φ 〈 47° (north of the equator). In this area geoid heights range between 42.157 m and 50.608 m, with an average of 46.162 m. The inner accuracy of the calculated geoid heights is 2.6 cm, the outer accuracy (based on 871 control GNSS/levelling measurements along levelling lines) is up to 10 cm. 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 ; Fast Fourier Transform ; Slovenia ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS 〉 GEOID CHARACTERISTICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
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  • 17
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    GFZRNX - RINEX GNSS Data Conversion and Manipulation Toolbox (Version 1.05) (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-02-03
    Description: Abstract
    Description: GFZRNX is a software toolbox for Global Navigation Satellite System (GNSS) data provided in the REceiver Independent EXchange format (RINEX) of the major versions 2 and 3. The following RINEX data types are supported: - Observation data - Navigation data - Meteorological dataThe following global and regional satellite systems are supported:GPS - Global Positioning System (USA) GLONASS - GLObal NAvigation Satellite System (RUS)BEIDOU - Chinese Global and Regional Navigation Satellite System (CHN)GALILEO - European Global Navigation Satellite SystemIRNSS - Indian Regional Naviagation Satellite System (IND)QZSS - Quasi Zenith Satellite System (JAP) The following operations/tasks are supported: - RINEX data check and repair - RINEX data format conversion ( version 3 to 2 and vice versa ) - RINEX data splice - RINEX data split - RINEX data statistics generation - RINEX data manipulations like: (1) data sampling, (2) observation types selection, (3) satellite systems selection, (4) elimination of overall empty or sparse observation types - Automatic version dependent file naming on output data - RINEX data header editing - RINEX data meta data extraction - RINEX data comparisonThe following operating systems are supported: - Microsoft Windows (64) - Microsoft Windows (32) - Apple macOS - ORACLE Solaris (SPARC) - ORACLE Solaris (i86) - Linux (64) - Linux (32) Please find the executables and the Documentation via: http://semisys.gfz-potsdam.de/semisys/scripts/download/index.php (GFZ Software -〉 gfzrnx)
    Keywords: RINEX ; GNSS ; GPS ; GLONASS ; GALILEO ; BEIDOU ; QZSS ; IRNSS
    Type: Software
    Format: 674121 Bytes
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    A new time series of GRACE monthly gravity field models: HUST-Grace2016 (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-03-03
    Description: Abstract
    Description: HUST-Grace2016 is a new time series of monthly gravity field models up to degree and order 60. The new HUST-Grace2016s is a new GRACE-only static gravity field model up to degree and order 160. Using about 13 years of GRACE Level 1B data spanning from January 2003 to April 2015. This new model has been developed by the institute of geophysics in the Huazhong University of Science and Technology (HUST). No constraint was applied. More details about our HUST-Grace2016s will be given in our paper “HUST-Grace2016s: a new GRACE static gravity field model derived from a modified dynamic approach over a 13-year observation period” (submitted to JGR Solid Earth in November 2016).This work is supported by the National Natural Science Foundation of China (No. 41131067, 41374023, 41474019), the Project funded by China Postdoctoral Science Foundation (No. 2016M592337).
    Description: Other
    Description: Input Data:- GRACE RL02 L1B (JPL) data products: January 2003 – March 2016- ITSG kinematic orbits: January 2003 – April 2015- AOD1B RL05 (GFZ) idealizing productCalculation method:- modified dynamic approach- numerical integrator: 14th-order Gauss-Jackson integrator- arc length: 24 hours- arc step: 5 secondsForce models:- Earth’s static gravity field: GGM05s up to degree and order 180- Ocean tides: EOT11a, truncated up to degree and order 120- N-body Perturbation: Direct and indirect J2 effects with JPL DE421- Solid earth tides: frequency independent/dependent terms, permanent tide- Solid earth tides: frequency independent/dependent terms, permanent tide- Pole tides: solid earth pole tides from IERS 2010, and ocean pole tides from Desai- Atmosphere and Oceanic variability: The AOD1B RL05 model up to degree 100- General Relativistic effects: IERS 2010
    Keywords: monthly gravity field model ; ICGEM ; geodesy
    Language: English
    Type: Dataset , Dataset
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  • 19
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    The Argentinian gravimetric geoid: GEOIDE-Ar16 (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-05-23
    Description: Abstract
    Description: The GEOIDE-Ar16 Argentinian gravimetric geoid model covers the area from 57° S to 20° S in latitude and from 76° W to 52° W in longitude, with a grid resolution of 1' × 1'. It was developed using the remove-compute-restore technique and incorporating the GOCO05S satellite-only global geopotential model up to degree and order 280, together with about 650,000 land and marine gravity measurements. Terrain corrections were calculated for all gravity observations using a combination of the SRTM_v4.1 and SRTM30_Plus_v10 digital elevation models. For the regions that lacked of gravity observations, the DTU13 gravity model was utilised. The residual gravity anomalies were gridded using the tensioned spline algorithm. The resultant gravity anomaly grid was applied in the Stokes' integral using the spherical multi-band FFT approach and the deterministic kernel modification proposed by Wong and Gore. The accuracy of GEOIDE-Ar16 was assessed by comparing it with GPS-levelling derived geoid undulations at 1,904 locations and the EGM2008 model. Results show that the GEOIDE-Ar16 geoid model has an accuracy of less than 10 centimetres. 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 ; Spherical multi-band Fast Fourier Transform ; Wong-Gore Stokes kernel modification ; Argentina ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS 〉 GEOID CHARACTERISTICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITY
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    Ground-based GPS observations at low elevation angles using open-loop signal tracking (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-06-05
    Description: Abstract
    Description: This data publication comprises (1) a one-year data set of ground-based GPS raw signal observations (inphase and quadphase C/A code correlation sums, NCO phases, pseudoranges) aiming at geometric elevation angles below +2°, (2) the "OpenGPS" receiver software and (3) MATLAB source code to access the raw data files. (1) ground-based GPS raw signal observations: Within the "GLESER" measurement campaign 2581 validated setting events were recorded by the "OpenGPS" open-loop tracking receiver at an observation site located at 52.3808°N, 13.0642°E (Potsdam, Germany) between January and December 2014. The instrument provided on average 8.3 observations per day with three data gaps (29 January to 1 February, 29–31 August and 18–22 December 2014) caused by hardware or software problems, operator errors or other technical reasons. Between 15 July and 6 September the "OpenGPS" receiver malfunctioned due to an operator error and 437 observations from that time period are removed from the data set leaving 2581 low-elevation events.Raw data files are stored in compressed tar archives each covering one week of observations. For more information see document "readme-gleser-dataset.pdf".(2) "OpenGPS" receiver software: The compressed tar archive "gleser-OpenGPS-src.tar.gz" includes (C code) sources of the OpenGPS receiver hardware. The receiver software is designed for "OpenSourceGPS"-compatible hardware (Kelley, 2002) and Linux operating system. During the 2014 campaign kernel version 2.6.32 (OpenSUSE version 11.3) with real-time extension module RTAI (RealTime Application Interface for Linux) version 3.8.1 was used. For more information see the document "readme-gleser-OpenGPS.pdf". (3) MATLAB source code: The compressed tar archive "gleser-readdata-src.tar.gz" contains a MATLAB function file that may be used to access the raw data files. For more information see the document "readme-gleser-readdata.pdf".
    Keywords: global navigation satellite system (GNSS) ; global positioning system (GPS) ; open-loop signal tracking ; atmospheric refractivity ; ground-based obervation
    Type: Dataset
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    The Combined Gravity Model GOCO05c (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-10-04
    Description: Abstract
    Description: GOCO05c is a static global combined gravity field model up to d/o 720. It has been elaborated by the GOCO Group (TU Munich, Bonn University, TU Graz, Austrian Academy of Sciences, University Bern). GOCO05c is a combination model based on the satellite-only gravity field model GOCO05s and several gravity anomaly datasets, constituting a global 15'x15' data grid. The combination is carried out in term of full normal equation systems.Contributing Institutions are: (1) TU Muenchen, DE, Institute of Astronomical and Physical Geodesy; (2) University of Bonn, DE, Institute of Geodesy and Geoinformation; (3) TU Graz, AU, Institute of Theoretical and Satellite Geodesy; (4) Austrian Academy of Sciences, Space Research Institute, and (5) University of Bern, CH, Astronomical Institute
    Description: Other
    Description: Global 15’x15’ data grid: Region (Source): Number of data cellsArctic (ArcGP Group): 44522Australia (Curtin University):11170Canada (NRCan):19259Europe (IfE Hanover):15625Oceans (DTU Space): 691818South America (NGA): 24818USA (NGA): 12895For the remaining land areas (Central America, Asia, Africa, Antarctica) fill-in datasets were used: Data (Source): Number of data cells NIMA96 (DMA/GSFC): 110594GOCO05s (GOCO Group): 106099 (band-limited gravity anomalies)RWI_TOIS2012 (KIT): 117737 (topographic anomalies)GOCO05c should not be used for geophysical applications in fill-in regions, because its high frequency part in fill-in regions resulted from simple synthetic numeric forward modelling of topographic information.
    Keywords: ICGEM ; global gravitational model ; GOCO ; Geodesy ; GOCE
    Language: English
    Type: Dataset , Dataset
    Format: 14167050 Bytes
    Format: 4 Files
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    The Combined Gravity Model GGM05C (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-10-04
    Description: Abstract
    Description: GGM05C is an unconstrained global gravity model complete to degree and order 360 determined from 1) GRACE K-band intersatellite range-rate data, GPS tracking and GRACE accelerometer data, 2) GOCE gradiometer data (ZZ+YY+XX+XZ) spanning the entire mission using a band pass filter of 10-50 mHz and polar gap filled with synthetic gradients from GGM05S to degree/order 150 evaluated at 200-km altitude, and 3) terrestrial gravity anomalies from DTU13 (Andersen et al., 2014). The value for C20 has been replaced with a value derived from satellite laser ranging. No rate terms were modeled. For additional details on the background modeling, see the CSR RL05 processing standards document available at ftp://podaac.jpl.nasa.gov/allData/grace/docs/L2-CSR0005_ProcStd_v4.0.pdf (Bettadpur 2012). Detailed information about GGM05C is available at ftp://ftp.csr.utexas.edu/pub/grace/GGM05/README_GGM05C.pdf (Ries et al., 2016).
    Keywords: ICGEM ; global gravitational model ; GRACE ; GOCE
    Language: English
    Type: Dataset , Dataset
    Format: 1734765 Bytes
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    EIGEN-6S4 A time-variable satellite-only gravity field model to d/o 300 based on LAGEOS, GRACE and GOCE data from the collaboration of GFZ Potsdam and GRGS Toulouse (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-10-04
    Description: Abstract
    Description: EIGEN-6S4 (Version 2) is a satellite-only global gravity field model from the combination of LAGEOS, GRACE and GOCE data. All spherical harmonic coefficients up to degree/order 80 are time variable. Their time variable parameters consist of drifts as well as annual and semi-annual variations per year. The time series of the time variable spherical harmonic coefficients are based on the LAGEOS-1/2 solution (1985 to 2003) and the GRACE-LAGEOS monthly gravity fields RL03-v2 (August 2002 to July 2014) from GRGS/Toulouse (Bruinsma et al. 2009).The herein included GRACE/LAGEOS data were combined with all GOCE data which have been processed via the direct numerical approach (Pail et al. 2011). The polar gap instabilty has been overcome using the Sperical Cap Regularization (Metzler and Pail 2005). That means this model is a combination of LAGEOS/GACE with GO_CONS_GCF_2_DIR_R5 (Bruinsma et al. 2013).Version History: This data set is an updated version of Foerste et al. (2016, http://doi.org/10.5880/icgem.2016.004) Compared to the first version, EIGEN-6S4v2 contains an improved modelling of the time variable part, in particular for C20.
    Keywords: ICGEM ; Global Gravitational Model ; GRACE ; GOCE ; LAGEOS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEODETICS 〉 GEOID CHARACTERISTICS ; EARTH SCIENCE 〉 SOLID EARTH 〉 GRAVITY/GRAVITATIONAL FIELD 〉 GRAVITATIONAL FIELD
    Type: Dataset
    Format: 8651697 Bytes
    Format: 3 Files
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  • 24
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    Spannungskarte Deutschland 2016 (2016)
    GFZ Data Services
    Details
    Publication Date: 2023-10-19
    Description: Abstract
    Description: Die Spannungskarte Deutschland zeigt die Orientierung der gegenwärtigen maximalen horizontalen Spannung (SHmax) in der Erdkruste. Unter der Annahme, dass die vertikale Spannung (SV) eine Hauptspannung ist, legt SHmax die Orientierung des 3D Spannungstensors festgelegt; die minimale horizontale Spannung Shmin ist entsprechend senkrecht zu SHmax. In der Spannungskarte sind die SHmax Orientierungen als Linien unterschiedlicher Länge dargestellt. Die Länge der Linie ist dabei ein Maß für die Datenqualität und das Symbol zeigt die Methode und die Farbe das Spannungsregime an. Daten mit E-Qualität sind ohne weitere Information als Punkte in der Karte dargestellt. Die Spannungsdaten sind frei zugänglich und Bestandteil des World Stress Map (WSM) Projektes. Weitere Informationen zu den Daten und Kriterien der Datenanalyse und Qualitätszuordnung befinden sich auf der WSM Internetseite unter http://www.world-stress-map.org. The English version of the World Stress Map Germany is available via http://doi.org/10.5880/WSM.Germany2016_en.
    Keywords: crustal stress ; in situ stress ; tectonic stress ; crustal stress pattern ; World Stress Map
    Type: Dataset
    Format: 9902687 Bytes
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  • 25
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    Sri Lanka temporary broadband network (2016)
    GFZ Data Services
    Details
    Publication Date: 2024-02-23
    Description: Abstract
    Description: A temporary seismic network was installed in Sri Lanka for a time period of 13 months. The stations were equipped with Earth Data EDR-210 digital recorders and Trillium 120 PA, Güralp C3E and Güralp CMG-3ESP broadband sensors. Main aim of the network is to shed light on the crustal and upper mantle structure beneath the island. Also local seismic activity is studied.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; 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
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    Array in Wittewierum, Netherlands (2016)
    GFZ Data Services
    Details
    Publication Date: 2024-02-23
    Description: Abstract
    Description: A temporary installation has been realized in the Netherlands, in the region of the Groningen gas field. The objective of this installation is to test the usage of a conventional array layout for detection of microseismicity. The region of the Groningen gas field is an excellent test ground, since the operating company NAM (Nederlandse Aardolie Maatschappij) installed a multitude of shallow borehole stations from 2014 to 2017, of which 65 – in addition to the already existing shallow borehole stations installed by KNMI (Koninklijk Nederlands Meteorologisch Instituut) – were already online during the time of measurement, thus ensuring an earthquake catalogue that is complete down to low magnitudes during the time of array installation. The site for the installation was decided together with local parties involved in the seismicity monitoring, i.e. KNMI and NAM, and was located close to the village of Wittewierum. Stations were installed from the 12th of July 2016 to the 29th of August 2016 (49 days). The array was composed of 9 stations. The array was constructed in three concentric rings of 75 m, 150 m and 225 m diameter including a central station, but the geometry had to be adapted to the local conditions. Each station consisted of a broadband sensor (Trillium 120 s), an acquisition system (CUBE datalogger), a battery, and a GPS antenna. The entire system was installed at ~1 m depth (apart from GPS and transmission antennas), requiring only the digging of shallow holes, one for the installation of a thin concrete plate and the sensor, another one for a box containing the remaining instrumentation. The array stations recorded continuously with little outages; only station WAR1 stopped recording on the 22nd of August and station WAR7 stopped recording from 20th to 22nd of August. Waveform data is available from the GEOFON data centre, under network code 1C, and is fully open.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; 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: ~30G
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    Lastarria volcano experiment (2016)
    GFZ Data Services
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    Publication Date: 2024-02-23
    Description: Abstract
    Description: The network consistes in 6 stations surronding the fumarole field at Lastarria volcano. These stations were operative during one month with the final purpose of detect changes in the hydrothermal system triggered by passing of seismic waves produced by artificial explosions. Waveform data are available from the GEOFON data centre, under network code 2G, and are embargoed until 001 2019.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; 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: approx. 9 GB
    Format: .mseed
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  • 28
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    Renland (2016)
    GFZ Data Services
    Details
    Publication Date: 2024-02-23
    Description: Abstract
    Description: The experiments are performed down the Edward Bailey valley, in the Renland peninsula, Scoresby Sund, Greenland. General purpose: ambient seismic noise recordings are obtained to characterize the geometry/structure of the valley the geometry/structure of the glaciers the microseismicity of the glacier, the friction process, crack orientation and mechanisms the seismic activity of glacial rivers, the relation between hydrological flow and noise spectrum the localization and characterization of sub-glacial flow from surface recordings. Seismic stations were composed of 3C broadband Trillium compact seismometer, a Cube datalogger and a 12V (D-cell types, stacked) battery pack.The experiment splits into three surveys performed at three different sites, one after the other, from july to august 2016. In the first experiment, we deploy 11 stations, 9 of them on a flat sandy area covering, partly, immobile ice that seems to be blocked between the Bailey Glacier (upstream) and the Apusinikajik glacier (downstream). The 9 sensors are placed a few hundreds of meters from the Apusinikajik lateral front, the last 2 are placed on the glacier next to the collapsing front. In the second and third experiment (chronologically speaking), we deploy 10 and 8 stations, respectively. Each deployment is performed along a Bailey valley transect. The first one intercepts the front-end of the glacier and the sub-glacial river exit (flow of several m3/s). The second transect is performed some 850m upstream. Waveform data are available from the GEOFON data centre, under network code 3H, and are embargoed until summer of 2019.
    Keywords: Seismic waveforms ; Monitoring system ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: Approximately 30 GB
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    Jailolo network, West Halmahera - Indonesia 2016/2018 (2016)
    GFZ Data Services
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    Publication Date: 2024-02-23
    Description: Abstract
    Description: The Halmahera island belongs to the North Moluccas province (Maluku Utara), Indonesia. This K-shaped island is located in the eastern part of the Moluccas Sea, the only active arc-arc collision complex on the Earth. The western arm of the K forms a volcanic arc due to the former subduction of the Moluccas Sea plate underneath Halmahera. The region is characterized by intense seismic activity at crustal, intermediate depth, and along the subducting plate. At crustal level the Halmahera seismicity along the two eastern arms of the K show strike-slip faulting style. In November 2015 a localized intense and energetic seismic activity started around Jailolo volcano in the West Halmahera Regency. The seismic sequence intermittently lasted until February 2016 and hundreds of events were felt by the population and several buildings were destroyed and damaged by the shaking. The largest shocks of the sequence have been located by global agencies (GEOFON and GCMT) showing normal faulting style. The temporal evolution of the seismicity seems to be more swarm-like type activity instead of mainshock-aftershock sequence. In spring 2016 a research project has been funded by the German's Humanitarian Aid program in collaboration with BMKG, Indonesia, with the goal of understanding the origin of the intense seismic activity and the related hazard. In summer 2016 we instrumented the area with a dense seismic network composed of 29 short period and 6 broad-band seismometers. The instruments deployment aims at characterizing the seismicity of the Jailolo region in relationship with the 2015-2016 seismic activity. The network will help to understand the seismo-tectonic of the area and the relation between seismicity and the volcanic activity at Jailolo volcano and possible link with the 2015-2016 swarm. Should the seismic activity intensify as in November 2015, we can record it and narrow down the underlying physical mechanisms. Waveform data are available from the GEOFON data centre, under network code 7G, and are embargoed until the end of 2021.
    Keywords: Broadband seismic waveforms ; Seismic monitoring ; 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: approx. 900GB
    Format: .mseed
    Format: XML
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    DATA GFZ
  • 30
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    Upper air soundings during POLARSTERN cruise PS96 (ANT-XXXI/2 FROSN) (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled balloons (TOTEX 600 g, 800 g) were used to carry Vaisala RS92-SGPW radiosondes. Whenever possible, the launches were performed about 10 UTC. Condensed measurements (TEMP Format FM-35) were transferred without delay into the Global Telecommunication System GTS were they contribute for the world wide weather forecasts. The profile data were taken every 5-10 seconds which result in a vertical profile resolution of about 25-50 meter. The profiles start at the helideck 10 m above sea level and terminate at the burst level of the balloons, normally at heights between 25 and 37 km.
    Keywords: AWI_Meteo; Meteorological Long-Term Observations @ AWI
    Type: Dataset
    Format: application/zip, 136 datasets
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  • 31
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    Bulk mineralogy and membership degrees of sediments from the Heihai lake area (2016)
    PANGAEA
    In:  Supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791, https://doi.org/10.1038/srep25791
    Details
    Publication Date: 2023-03-13
    Description: Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asia. Paleoclimatic evidence, however, suggests increased moisture availability in the Early Holocene north of the Himalayan range which is attributed to an intensification of the Indian Summer Monsoon. Nevertheless, mechanisms leading to a surpassing of the Himalayan range and the northern maximum extent of summer monsoonal influence remain unknown. Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer Monsoon which is persistent throughout the Holocene. Precipitation intensities at its northern extent seem to be driven by differentiated solar heating of the Northern Hemisphere indicating dependency on energy-gradients rather than absolute radiation intensities. The identified spatial constraints of monsoonal precipitation will facilitate the prediction of future monsoonal precipitation patterns in Central Asia under varying climatic conditions.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/zip, 17 datasets
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  • 32
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    (Appendix 3) General and physico-chemical characteristics of monitoring site Pok-01 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; AWI_PerDyn; AWI_POK-01; AWI Arctic Land Expedition; Bottom water temperature; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; DEPTH, water; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; Monitoring station; MONS; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Siberia, Russia; Temperature, air; Temperature, water; Thaw depth of active layer
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 33
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    (Appendix 8-3) Soil description and pH measurements of the pingo 'Shirokovsky Kholm' (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI_Pi01; AWI_Pi02; AWI_Pi03; AWI_Pi04; AWI_Pi05; AWI_Pi06; AWI_Pi07; AWI_Pi08; AWI_Pi09; AWI_Pi10; AWI_Pi11; AWI_Pi12; AWI_Pi13; AWI_Pi14; AWI_PiL; AWI Arctic Land Expedition; DEPTH, soil; Depth, soil, maximum; Depth, soil, minimum; East Siberia; Event label; islet1; islet2.center; islet2.wall; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Soil horizon; Soil type
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 34
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    Physical oceanography of CTD station CTD_20140822 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20140822; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 22440 data points
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  • 35
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    Physical oceanography of CTD station CTD_20150828 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20150828; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 46315 data points
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    DATA PANGAEA
  • 36
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    Molecular fingerprinting and amplicon sequencing of the bacterial biofilm on settlement tiles deployed along natural pH gradients in Papua New Guinea : environmental data (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: BIOACID; BIOACID 2 PNG2013; Biological Impacts of Ocean Acidification; DATE/TIME; DIVER; Environment; LATITUDE; Layer description; Location; LONGITUDE; M.V. Chertan; Number; Papua_New_Guinea_CO2_vent; pH; Sample code/label; Sample ID; Sampling by diver
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 37
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    Experimental results for Ecklonia radiata in situ incubation experiment (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Change; Darlington; DATE/TIME; EXP; Experiment; Oxygen saturation; pH; pH change; Replicate; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 168 data points
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  • 38
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    In situ measurements of pH within E. radiata beds in south eastern Tasmania (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Darlington; DATE/TIME; DEPTH, water; Event label; EXP; Experiment; Fortescue_Bay; Habitat; LATITUDE; LONGITUDE; Oxygen; pH; ph electrode; pHTempion; Replicate; Salinity; SeaPHOX; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 9497 data points
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  • 39
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    (Fig. 2c) Membership degrees of Heihai catchment sediments to mineralogical cluster C1 to C4 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Calculated; China2011,China2012/1,China2012/2,China2012/3; Cluster membership; CN-Land_2012; Date/Time of event; DEPTH, sediment/rock; Event label; HAND; HH-11154; HH-11163; HH-11192; HH-11199; HH-11211; HH-11278; HH-11285; HH-11286; HH-11287; HH-11316; HH-2012-08-20-001; HH-2012-08-20-003; HH-2012-08-20-004; HH-2012-08-20-005; HH-2012-08-20-006; HH-2012-08-20-007; HH-2012-08-20-008; HH-2012-08-20-010; HH-2012-08-20-011; HH-2012-08-20-012; HH-2012-08-20-013; HH-2012-08-20-014; HH-2012-08-20-016; HH-2012-08-20-017a; HH-2012-08-20-017b; HH-2012-08-20-018; HH-2012-08-20-019; HH-2012-08-20-020; HH-2012-08-20-021; HH-2012-08-20-022; HH-2012-08-20-023a; HH-2012-08-20-023b; HH-2012-08-20-024; HH-2012-08-20-025; HH-2012-08-20-029; HH-2012-08-21-001; HH-2012-08-21-002; HH-2012-08-21-004; HH-2012-08-21-006; HH-2012-08-21-007; HH-2012-08-21-008; HH-2012-08-21-009; HH-2012-08-23-001; HH-2012-08-23-004; HH-2012-08-23-006; HH-2012-08-23-007; HH-2012-08-23-008; HH-2012-08-23-009b; HH-2012-08-23-010; HH-2012-08-23-011; HH-2012-08-23-012; HH-9739; HH-9912; HH-9914; HH-9918; HH-9919; HH-9951; HH-9952; Lake Heihai, Qinghai, China; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling by hand
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 40
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    Hydrochemistry measured on water bottle samples during cruise Dana01/16 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Keywords: Chlorophyll total; CTD/Rosette; CTD-RO; Dana01/16; Dana01/16_103; Dana01/16_104; Dana01/16_105; Dana01/16_106; Dana01/16_113; Dana01/16_114; Dana01/16_117; Dana01/16_118; Dana01/16_119; Dana01/16_127; Dana01/16_128; Dana01/16_129; Dana01/16_137; Dana01/16_138; Dana01/16_139; Dana01/16_141; Dana01/16_142; Dana01/16_148; Dana01/16_149; Dana01/16_150; Dana01/16_151; Dana01/16_160; Dana01/16_161; Dana01/16_162; Dana01/16_163; Dana01/16_171; Dana01/16_172; Dana01/16_177; Dana01/16_178; Dana01/16_179; Dana01/16_180; Dana01/16_186; Dana01/16_187; Dana01/16_188; Dana01/16_189; Dana01/16_197; Dana01/16_198; Dana01/16_199; Dana01/16_200; Dana01/16_207; Dana01/16_208; Dana01/16_209; Dana01/16_210; Dana01/16_213; Dana01/16_214; Dana01/16_215; Dana01/16_216; Dana II; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Kattegat; Latitude of event 2; Longitude of event; Nitrate; Nitrite; Nitrogen, total; Oxygen; Phosphate; Phosphorus, total; Pressure, water; Salinity; Silicate; Skagerrak; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2654 data points
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  • 41
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    Physical oceanography during cruise Scotia16/1 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Norwegian Sea; Pressure, water; Salinity; Scotia; Scotia16/1; Scotia16/1_10; Scotia16/1_11; Scotia16/1_12; Scotia16/1_13; Scotia16/1_14; Scotia16/1_15; Scotia16/1_16; Scotia16/1_17; Scotia16/1_18; Scotia16/1_19; Scotia16/1_20; Scotia16/1_21; Scotia16/1_22; Scotia16/1_23; Scotia16/1_24; Scotia16/1_25; Scotia16/1_26; Scotia16/1_27; Scotia16/1_28; Scotia16/1_29; Scotia16/1_30; Scotia16/1_31; Scotia16/1_32; Scotia16/1_33; Scotia16/1_34; Scotia16/1_35; Scotia16/1_36; Scotia16/1_37; Scotia16/1_38; Scotia16/1_39; Scotia16/1_40; Scotia16/1_41; Scotia16/1_42; Scotia16/1_43; Scotia16/1_44; Scotia16/1_45; Scotia16/1_46; Scotia16/1_47; Scotia16/1_48; Scotia16/1_49; Scotia16/1_50; Scotia16/1_51; Scotia16/1_52; Scotia16/1_53; Scotia16/1_9; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2688 data points
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  • 42
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    Hydrochemical properties of groundwater samples in Semarang area, Java Island, Indonesia (1992, 1993, 2003, 2006, and 2007) (2016)
    PANGAEA
    In:  Supplement to: Putranto, Thomas Triadi; Rüde, Thomas (2016): Hydrogeological model of an urban city in a coastal area, case study: Semarang, Indonesia. Indonesian Journal on Geoscience, 3(1), 17-27, https://doi.org/10.17014/ijog.3.1.17-27
    Details
    Publication Date: 2023-03-14
    Description: In Semarang City, groundwater has been exploited as a natural resource since 1841. The groundwater exploited in deep wells is concentrated in confined aquifers. The previous hydrogeological model was developed in one unit of aquifer and refined then by using several hydrostratigraphical units following a regional hydrogeological map without any further analysis. At present, there is a lack of precise hydrogeological model which integrates geological and hydrogeological data, in particular for multiple aquifers in Semarang. Thus, the aim of this paper is to develop a hydrogeological model for the multiple aquifers in Semarang using an integrated data approach. Groundwater samples in the confined aquifers have been analyzed to define the water type and its lateral distribution. Two hydrogeological cross sections were then created based on several borelog data to define a hydrostratigraphical unit (HSU). The HSU result indicates the hydrogeological model of Semarang consists of two aquifers, three aquitards, and one aquiclude. Aquifer 1 is unconfined, while Aquifer 2 is confined. Aquifer 2 is classified into three groups (2a, 2b, and 2c) based on analyses of major ion content and hydrostratigraphical cross sections.
    Keywords: Aquifer type; Area/locality; Balance; Bicarbonate ion; Calcium; Calculated; Chloride; Conductivity, electrical; DATE/TIME; Depth, well; ELEVATION; Event label; Facies name/code; Handheld GPS, Garmin; Java Island, northern coast; Latitude of event; Longitude of event; Magnesium; N_1; N_2; N_3; N_7; pH; Portable water detector; Portable water quality meter (Hanna Instruments); Potassium; Sample position; Sampling Well; SB_100; SB_112; SB_120; SB_176; SB_185; SB_189; SB_190; SB_198; SB_206; SB_210; SB_211; SB_213; SB_214; SB_215; SB_217; SB_219; SB_220; SB_225; SB_226; SB_235; SB_256; SB_262; SB_265; SB_270; SB_271; SB_273; SB_278; SB_281; SB_282; SB_283; SB_297; SB_299; SB_321; SB_325; SB_33; SB_332; SB_344; SB_347; SB_348; SB_36; SB_590; SB_60; SB_726; SB_758; SB_790; SB_793; SB_92; SB_951; Sodium; SP_136; SP_138; SP_139; SP_341; SP_342; SP_764; Spectrophotometric; Sulfate; Total dissolved solids; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Water level; WELL
    Type: Dataset
    Format: text/tab-separated-values, 1131 data points
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  • 43
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    Hydrography measured in lakes during the North Yakutia expedition in 2006 (2016)
    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Details
    Publication Date: 2023-03-14
    Keywords: 06-CYak-01; 06-CYak-02; 06-CYak-03; 06-CYak-04; 06-CYak-05; 06-NYak-01; 06-NYak-02; 06-NYak-03; 06-NYak-04; 06-NYak-05; 06-NYak-06; 06-NYak-07; 06-NYak-08; 06-NYak-09; 06-NYak-10; 06-NYak-11; 06-NYak-12; 06-NYak-13; 06-NYak-14; 06-NYak-15; Alaas; AWI_PerDyn; AWI Arctic Land Expedition; Ayan; Central Yakutia, Russia; Chat; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Dulla; Etektyak; Event label; Ilimniir; Ivanovka; Kerdugen; Ketitiki; Krestyak; Latitude of event; Longitude of event; MULT; Multiple investigations; Nami-Kuel; North_Yakutia_2006; North Yakutia, Russia; Oibon-Kuel; Oloror; Oppoyao; Optional event label; Otto; Oxygen; Oxygen saturation; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2006_Yakutia; Spasskoe; Suturuoka; Temperature, water; Thee-Bihii; Timpi; Ushepes
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 44
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    Hydrography measured in lakes during the Tiksi expedition in 2009 (2016)
    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Details
    Publication Date: 2023-03-14
    Keywords: 09-TIK-01; 09-TIK-02; 09-TIK-03; 09-TIK-04; 09-TIK-05; 09-TIK-08; 09-TIK-09; 09-TIK-10; 09-TIK-11; 09-TIK-12; 09-TIK-13; 09-TIK-14; Alkalinity, total; AWI_PerDyn; AWI Arctic Land Expedition; Byluyng Kjuel; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Elgene Kjuel; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2009_Lena-transect; Tiksi2009; Vegetation type
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 45
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    Hydrochemistry measured on water bottle samples during Dalniye Zelentsy cruise 90BYBA40 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90BYBA40; 90BYBA40-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 7172 data points
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  • 46
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    Hydrochemistry measured on water bottle samples during Professor Deryugin cruise 90PD9E40 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90PD9E40; 90PD9E40-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 4574 data points
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  • 47
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    Hydrochemistry measured on water bottle samples during DIANA cruise 90DI9D20 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90DI9D20; 90DI9D20-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1941 data points
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  • 48
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    Hydrochemistry measured on water bottle samples during Professor Deryugin cruise 90PD9F70 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90PD9F70; 90PD9F70-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 380 data points
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  • 49
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    Hydrochemistry measured on water bottle samples during Professor Deryugin cruise 90PD9F50 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90PD9F50; 90PD9F50-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1018 data points
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  • 50
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    Hydrochemistry measured on water bottle samples during Professor Deryugin cruise 90PD9F80 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90PD9F80; 90PD9F80-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 9627 data points
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  • 51
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    Hydrochemistry measured on water bottle samples at coastal station Kola Bay in 2000 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90SBC810; 90SBC810-track; Ammonium; Coastal station Kola Bay; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 2939 data points
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  • 52
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    Hydrochemistry measured on water bottle samples during cruise 90XX9BA0 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90XX9BA0; 90XX9BA0-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 282 data points
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  • 53
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    Hydrochemistry measured on water bottle samples during cruise 90XX9C20 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90XX9C20; 90XX9C20-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 283 data points
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  • 54
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    Hydrochemistry measured on water bottle samples during ARANDA cruise 34AR9D7A (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 34AR9D7A; 34AR9D7A-track; Alkalinity, total; Ammonium; Aranda (1953); CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 5073 data points
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  • 55
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    Bacteria growth, enzyme activities and TEP during KOSMOS 2011 mesocosm experiment in the Raunefjord (2016)
    PANGAEA
    In:  Supplement to: Endres, Sonja; Galgani, Luisa; Riebesell, Ulf; Schulz, Kai Georg; Engel, Anja (2014): Stimulated Bacterial Growth under Elevated pCO2: Results from an Off-Shore Mesocosm Study. PLoS ONE, 9(6), e99228, https://doi.org/10.1371/journal.pone.0099228
    Details
    Publication Date: 2023-03-14
    Description: Marine bacteria are the main consumers of freshly produced organic matter. Many enzymatic processes involved in the bacterial digestion of organic compounds were shown to be pH sensitive in previous studies. Due to the continuous rise in atmospheric CO2 concentration, seawater pH is presently decreasing at a rate unprecedented during the last 300 million years but the consequences for microbial physiology, organic matter cycling and marine biogeochemistry are still unresolved. We studied the effects of elevated seawater pCO2 on a natural plankton community during a large-scale mesocosm study in a Norwegian fjord. Nine Kiel Off-Shore Mesocosms for Future Ocean Simulations (KOSMOS) were adjusted to different pCO2 levels ranging initially from ca. 280 to 3000 µatm and sampled every second day for 34 days. The first phytoplankton bloom developed around day 5. On day 14, inorganic nutrients were added to the enclosed, nutrient-poor waters to stimulate a second phytoplankton bloom, which occurred around day 20. Our results indicate that marine bacteria benefit directly and indirectly from decreasing seawater pH. During the first phytoplankton bloom, 5-10% more transparent exopolymer particles were formed in the high pCO2 mesocosms. Simultaneously, the efficiency of the protein-degrading enzyme leucine aminopeptidase increased with decreasing pH resulting in up to three times higher values in the highest pCO2/lowest pH mesocosm compared to the controls. In general, total and cell-specific aminopeptidase activities were elevated under low pH conditions. The combination of enhanced enzymatic hydrolysis of organic matter and increased availability of gel particles as substrate supported up to 28% higher bacterial abundance in the high pCO2 treatments. We conclude that ocean acidification has the potential to stimulate the bacterial community and facilitate the microbial recycling of freshly produced organic matter, thus strengthening the role of the microbial loop in the surface ocean.
    Keywords: Abundance per volume; BIOACID; Biological Impacts of Ocean Acidification; Chlorophyll a; DATE/TIME; Day of experiment; KOSMOS_2011_Bergen; Leucine aminopeptidase activity; MESO; Mesocosm experiment; pH; Raunefjord; Sample code/label; Transparent exopolymer particles as Gum Xanthan equivalents per volume; Transparent exopolymer particles as Gum Xanthan equivalents per volume, std dev
    Type: Dataset
    Format: text/tab-separated-values, 2053 data points
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  • 56
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    Physical oceanography of CTD station CTD_20120822_st1 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 23155 data points
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  • 57
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    Physical oceanography of CTD station CTD_20120822_st3 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St3; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 9960 data points
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  • 58
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    Physical oceanography of CTD station CTD_20120828_st1 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 12530 data points
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  • 59
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    Physical oceanography of CTD station CTD_20130904 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20130904; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 31030 data points
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  • 60
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    Physical oceanography of CTD station CTD_20120828_st4 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St4; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 1635 data points
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  • 61
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    Calcification repsonse of marine bivalves to changed carbonate chemistry: Carbonate system (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Carbon, inorganic, dissolved; Carbonate ion; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Ratio; Salinity; Sample code/label; Standard deviation; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 506 data points
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  • 62
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    (Appendix 4) General and physico-chemical characteristics of the studied ponds and lakes POK-02 to POK-31 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; Area/locality; AWI_PerDyn; AWI_POK-02; AWI_POK-03; AWI_POK-04; AWI_POK-05; AWI_POK-06; AWI_POK-07; AWI_POK-08; AWI_POK-09; AWI_POK-10; AWI_POK-11; AWI_POK-12; AWI_POK-13; AWI_POK-14; AWI_POK-15; AWI_POK-16; AWI_POK-17; AWI_POK-18; AWI_POK-19; AWI_POK-20; AWI_POK-21; AWI_POK-22; AWI_POK-23; AWI_POK-24; AWI_POK-25; AWI_POK-26; AWI_POK-27; AWI_POK-28; AWI_POK-29; AWI_POK-30; AWI_POK-31; AWI Arctic Land Expedition; Bottom water temperature; Comment; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; Event label; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Size; Temperature, air; Temperature, water; Type
    Type: Dataset
    Format: text/tab-separated-values, 445 data points
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  • 63
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    (Appendix 8-1+2) Sample description and field data of the pingo exposure 'Shirokovsky Kholm' (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrolytic; DEPTH, sediment/rock; Description; Distance; East Siberia; Height; Ice content; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Permafrost Research (Periglacial Dynamics) @ AWI; pH; pingo_exposure; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sample type; Sampling/measurement on land; Shirokovsky_Kholm
    Type: Dataset
    Format: text/tab-separated-values, 437 data points
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  • 64
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    (Appendix 5-1) Field measurements of limnological samples (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: AWI_L-24; AWI_L-25; AWI_L-31; AWI_L-34; AWI_L-36; AWI_L-38; AWI_L-6; AWI_L-62; AWI_L-66; AWI_L-80; AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrical; DATE/TIME; DEPTH, water; Event label; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Siberia, Russia
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 65
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    Physical oceanography of CTD station CTD_20120822_st2 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 19395 data points
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  • 66
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    Physical oceanography of CTD station CTD_20120828_st2 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 10530 data points
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  • 67
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    Hydrochemistry measured on water bottle samples during POMOR cruise 9038B970 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 9038B970; 9038B970-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Pomor; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1000 data points
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  • 68
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    Hydrochemistry measured on water bottle samples during Dalniye Zelentsy cruise 90BYB8C0 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90BYB8C0; 90BYB8C0-track; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1307 data points
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  • 69
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    Hydrochemistry measured on water bottle samples during Dalniye Zelentsy cruise 90BYBA60 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90BYBA60; 90BYBA60-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1687 data points
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  • 70
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    Hydrochemistry measured on water bottle samples during DIANA cruise 90DI9CA0 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90DI9CA0; 90DI9CA0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1181 data points
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  • 71
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    Hydrochemistry measured on water bottle samples during DIANA cruise 90DI9D10 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90DI9D10; 90DI9D10-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 929 data points
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  • 72
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    Hydrochemistry measured on water bottle samples during DIANA cruise 90DI9CB0 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: 90DI9CB0; 90DI9CB0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1623 data points
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  • 73
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    Dissolved organic sulfur in solid-phase extracts of water samples obtained during POLARSTERN cruise ANT-XXV (PS73) (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Age, 14C; Age, dated; ANT-XXV/1; ANT-XXV/2; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Carbon, organic, dissolved; Carbon, organic, dissolved, extracted; Celtic Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Ecological Chemistry @ AWI; English Channel; Event label; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Nitrogen, organic, dissolved, extracted; Polarstern; PS73; PS73/002-1; PS73/004-1; PS73/006-1; PS73/006-3; PS73/008-1; PS73/010-2; PS73/013-1; PS73/015-1; PS73/015-2; PS73/017-2; PS73/019-1; PS73/022-1; PS73/024-1; PS73/026-1; PS73/026-2; PS73/028-1; PS73/030-1; PS73/032-1; PS73/032-4; PS73/034-1; PS73/036-1; PS73/038-1; PS73/038-2; PS73/042-1; PS73/044-1; PS73/047-1; PS73/051-1; PS73/054-1; PS73/056-1; PS73/062-1; PS73/064-1; PS73/069-2; PS73/070-1; PS73/071-1; PS73/072-1; PS73/073-1; PS73/074-1; PS73/S10; PS73/S11; PS73/S13; PS73/S15; PS73/S16; PS73/S17; PS73/S19; PS73/S2; PS73/S21; PS73/S24; PS73/S26; PS73/S29; PS73/S3; PS73/S30; PS73/S32; PS73/S34; PS73/S36; PS73/S38; PS73/S41; PS73/S43; PS73/S44; PS73/S45; PS73/S46; PS73/S47; PS73/S49; PS73/S5; PS73/S50; PS73/S52; PS73/S55; PS73/S57; PS73/S58; PS73/S60; PS73/S66; PS73/S67; PS73/S68; PS73/S69; PS73/S7; PS73/S70; PS73/S71; PS73/SW1; PS73/SW10; PS73/SW11; PS73/SW12; PS73/SW13; PS73/SW14; PS73/SW15; PS73/SW16; PS73/SW17; PS73/SW18; PS73/SW19; PS73/SW2; PS73/SW3; PS73/SW4; PS73/SW5; PS73/SW6; PS73/SW7; PS73/SW8; PS73/SW9; RAMSES; RAMSES hyperspectral radiometer; Solid phase extraction (SPE) with PPL sorbent (after Flerus et al. 2012); South Atlantic Ocean; Station label; Sulfur, organic, dissolved, extracted; Sulfur, organic, dissolved/Nitrogen, organic, dissolved ratio; Surface water sample; SWS; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1234 data points
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  • 74
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    Molecular characterization of sulfur-containing compounds in solid-phase extracts of water samples obtained during POLARSTERN cruise ANT-XXV (PS73) (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ANT-XXV/1; ANT-XXV/2; Area/locality; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Celtic Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Double bond equivalent; Ecological Chemistry @ AWI; English Channel; Event label; Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS); Hydrogen/Carbon ratio; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Mass of molecular formulas; Nitrogen/Carbon ratio; Oxygen/Carbon ratio; Polarstern; PS73; PS73/002-1; PS73/004-1; PS73/006-1; PS73/006-3; PS73/008-1; PS73/010-2; PS73/013-1; PS73/015-1; PS73/015-2; PS73/017-2; PS73/019-1; PS73/022-1; PS73/024-1; PS73/026-1; PS73/026-2; PS73/028-1; PS73/030-1; PS73/032-1; PS73/032-4; PS73/034-1; PS73/036-1; PS73/038-1; PS73/038-2; PS73/042-1; PS73/044-1; PS73/047-1; PS73/051-1; PS73/054-1; PS73/056-1; PS73/064-1; PS73/069-2; PS73/070-1; PS73/071-1; PS73/072-1; PS73/073-1; PS73/074-1; PS73/S10; PS73/S11; PS73/S13; PS73/S15; PS73/S16; PS73/S17; PS73/S19; PS73/S2; PS73/S21; PS73/S24; PS73/S26; PS73/S29; PS73/S3; PS73/S30; PS73/S32; PS73/S34; PS73/S36; PS73/S38; PS73/S41; PS73/S43; PS73/S44; PS73/S45; PS73/S46; PS73/S47; PS73/S49; PS73/S5; PS73/S52; PS73/S55; PS73/S57; PS73/S58; PS73/S60; PS73/S66; PS73/S67; PS73/S68; PS73/S69; PS73/S7; PS73/S70; PS73/S71; PS73/SW1; PS73/SW10; PS73/SW11; PS73/SW12; PS73/SW13; PS73/SW14; PS73/SW15; PS73/SW16; PS73/SW17; PS73/SW18; PS73/SW19; PS73/SW2; PS73/SW3; PS73/SW4; PS73/SW5; PS73/SW6; PS73/SW7; PS73/SW8; PS73/SW9; RAMSES; RAMSES hyperspectral radiometer; South Atlantic Ocean; Station label; Sulfur/Carbon ratio; Surface water sample; SWS; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1400 data points
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  • 75
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    Methionine-sulfur yield of two depth profiles of solid-phase extractable dissolved organic matter obtained during POLARSTERN cruise ANT-XXV (PS73) (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ANT-XXV/1; ANT-XXV/2; Area/locality; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Ecological Chemistry @ AWI; Event label; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Methionine; Polarstern; PS73; PS73/026-1; PS73/026-2; PS73/073-1; Solid phase extraction (SPE) with PPL sorbent (after Flerus et al. 2012); Station label; Sulfur, organic, dissolved, extracted; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 76
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    Raw data of SCADCP (self-contained Acoustic Doppler Current Profiler) from mooring AWI229-7 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI229-7; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 285.7 MBytes
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  • 77
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    Raw data of SCADCP (self-contained Acoustic Doppler Current Profiler) from mooring AWI231-7 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI231-7; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 287.1 MBytes
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  • 78
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    Raw data of SCADCP (self-contained Acoustic Doppler Current Profiler) from mooring AWI232-8 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI232-8; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 306.2 MBytes
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  • 79
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    Positioning of ROV at station PS92/019-6 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/019-6; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 35946 data points
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  • 80
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    Positioning of ROV at station PS92/031-2 (2016)
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    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/031-2; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 34890 data points
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  • 81
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/027-2 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/027-2; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 32268 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 82
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/032-4 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/032-4; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 26568 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 83
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/039-6 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/039-6; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 38490 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 84
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/043-4 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/043-4; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 32334 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 85
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/046-1 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/046-1; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 52356 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 86
    facet.materialart.
    Unknown
    Positioning of ROV at station PS92/047-3 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Distance to sea-ice bottom; Heading; ICE; Ice station; Pitch angle; Polarstern; PS92; PS92/047-3; Roll angle; Sea Ice Physics @ AWI
    Type: Dataset
    Format: text/tab-separated-values, 30174 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 87
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/019-6 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/019-6; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2916400 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 88
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/027-2 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/027-2; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2357212 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 89
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/039-6 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/039-6; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 512272 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 90
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/031-2 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/031-2; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 4226244 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 91
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/043-4 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/043-4; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2783260 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 92
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/046-1 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/046-1; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 687256 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 93
    facet.materialart.
    Unknown
    Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at ROV station PS92/047-3 (2016)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/047-3; Sea Ice Physics @ AWI; Transflectance; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 3376684 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 94
    facet.materialart.
    Unknown
    Radiosonde PS98/38786 during POLARSTERN cruise PS98 (ANT-XXXI/4) on 2016-04-29 10:44h (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38786; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6125 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 95
    facet.materialart.
    Unknown
    Radiosonde PS98/38788 during POLARSTERN cruise PS98 (ANT-XXXI/4) on 2016-04-30 02:58h (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38788; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6780 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 96
    facet.materialart.
    Unknown
    Radiosonde PS98/38794 during POLARSTERN cruise PS98 (ANT-XXXI/4) on 2016-05-06 10:36h (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38794; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 5790 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 97
    facet.materialart.
    Unknown
    Radiosonde PS98/38796 during POLARSTERN cruise PS98 (ANT-XXXI/4) on 2016-05-08 10:32h (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38796; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6480 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 98
    facet.materialart.
    Unknown
    Dive depth profile of Weddell seal FIL2014_wed_a_f_06 from Filchner Trough (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_06; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-07-13
    Type: Dataset
    Format: text/tab-separated-values, 73203 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 99
    facet.materialart.
    Unknown
    Dive depth profile of Weddell seal FIL2014_wed_a_m_03 from Filchner Trough (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_m_03; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-03-13
    Type: Dataset
    Format: text/tab-separated-values, 26429 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 100
    facet.materialart.
    Unknown
    Dive depth profile of Weddell seal FIL2014_wed_a_f_01 from Filchner Trough (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_01; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-01-13
    Type: Dataset
    Format: text/tab-separated-values, 41145 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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