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  • Elsevier  (13,839)
  • PANGAEA  (7,751)
  • American Physical Society
  • 2020-2024  (21,681)
  • 1960-1964
  • 1955-1959
  • 2021  (21,681)
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  • 1
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    How a water-resources crisis highlights social-ecological disconnects (2021)
    Elsevier
    In:  EPIC3Water Research, Elsevier, 194, pp. 116937-116937, ISSN: 0043-1354
    Details
    Publication Date: 2023-10-04
    Description: The sustainable management of water resources is required to avoid water scarcity becoming widespread. This article explores the potential application of a social-ecological framework, used predominantly in the fields of ecology and conservation, as a tool to improve the sustainability and resilience of water resources. The "red-loop green-loop" (RL-GL) model has previously been used to map both sustainable and unsustainable social-ecological feedbacks between ecosystems and their communities in countries such as Sweden and Jamaica. In this article, we demonstrate the novel application of the RL-GL framework to water resources management using the 2017/18 Cape Town water crisis. We used the framework to analyse the social-ecological dynamics of pre-crisis and planned contingency scenarios. We found that the water resources management system was almost solely reliant on a single, non-ecosystem form of infrastructure, the provincial dam system. As prolonged drought impacted this key water resource, resilience to resource collapse was shown to be low and a missing feedback between the water resource and the Cape Town community was highlighted. The collapse of water resources ("Day Zero") was averted through a combination of government and community group led measures, incorporating both local ecosystem (green-loop) and non-local ecosystem (red-loop) forms of water resource management, and increased rainfall returning to the area. Additional disaster management plans proposed by the municipality included the tighter integration of red and green-loop water management approaches, which acted to foster a stronger connection between the Cape Town community and their water resources. We advocate the wider development and application of the RL-GL model, theoretically and empirically, to investigate missing feedbacks between water resources and their communities.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 2
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    Leverage points for addressing marine and coastal pollution: A review (2021)
    Elsevier
    In:  EPIC3Marine Pollution Bulletin, Elsevier, 167, pp. 112263-112263, ISSN: 0025-326X
    Details
    Publication Date: 2023-10-04
    Description: Despite an increasing understanding of the issue of marine pollution, humanity continues on a largely unsustainable trajectory. This study aimed to identify and classify the range of scientific studies and interventions to address coastal and marine pollution. We reviewed 2417 scientific papers published between 2000 and 2018, 741 of which we analysed in depth. To classify pollution interventions, we applied the systems-oriented concept of leverage points, which focuses on places to intervene in complex systems to bring about systemic change. We found that pollution is largely studied as a technical problem and fewer studies engage with pollution as a systemic social-ecological issue. While recognising the importance of technical solutions, we highlight the need to focus on under-researched areas pertaining to the deeper drivers of pollution (e.g. institutions, values) which are needed to fundamentally alter system trajectories.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
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    Late Holocene Ameghinomya antiqua shells from the Beagle Channel: A multi-proxy approach to palaeoenvironmental and palaeoclimatic reconstruction (2021)
    Elsevier
    In:  EPIC3Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 578, pp. 110574
    Details
    Publication Date: 2023-03-13
    Description: It is important to understand the historical precedents of current situations to be able to anticipate where the current global environmental and climatic change may lead. Geo-historical data provide information beyond the limitations of instrumental data. This study aims to reconstruct components of the palaeoclimatic and palaeoenvironmental history of the Beagle Channel (BC) during the Late Holocene by using Ameghinomya antiqua shells. We use fossil and modern shells in a comparative analysis through a multiproxy approach, i.e., shell morphometrics, shell growth, and stable oxygen isotope ratios. A holistic analysis of all the proxies indicates that higher productivity occurred around 3542 yr B.P. in the BC, evidenced by more significant growth, size, and longevity in fossil specimens. In addition, smaller ligaments, cardinal teeth, and the pallial sinus in fossil specimens indicate a low-energy environment typical of a marine archipelago. Lastly, palaeotemperatures are estimated to be warmer than today, although the intensity may be overestimated due to the freshwater inflow that would change the salinity of the BC waters. Further analysis in Late-Holocene shells is essential for a more detailed environmental reconstruction around the southern tip of South America.
    Repository Name: EPIC Alfred Wegener Institut
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  • 4
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    Harmful algal blooms and their effects in coastal seas of Northern Europe (2021)
    Elsevier
    In:  EPIC3Harmful Algae, Elsevier, pp. 101989, ISSN: 15689883
    Details
    Publication Date: 2023-03-13
    Description: Harmful algal blooms (HAB) are recurrent phenomena in northern Europe along the coasts of the Baltic Sea, Kattegat-Skagerrak, eastern North Sea, Norwegian Sea and the Barents Sea. These HABs have caused occasional massive losses for the aquaculture industry and have chronically affected socioeconomic interests in several ways. This status review gives an overview of historical HAB events and summarises reports to the Harmful Algae Event Database from 1986 to the end of year 2019 and observations made in long term monitoring programmes of potentially harmful phytoplankton and of phycotoxins in bivalve shellfish. Major HAB taxa causing fish mortalities in the region include blooms of the prymnesiophyte Chrysochromulina leadbeateri in northern Norway in 1991 and 2019, resulting in huge economic losses for fish farmers. A bloom of the prymesiophyte Prymnesium polylepis (syn. Chrysochromulina polylepis) in the Kattegat-Skagerrak in 1988 was ecosystem disruptive. Blooms of the prymnesiophyte Phaeocystis spp. have caused accumulations of foam on beaches in the southwestern North Sea and Wadden Sea coasts and shellfish mortality has been linked to their occurrence. Mortality of shellfish linked to HAB events has been observed in estuarine waters associated with influx of water from the southern North Sea. The first bloom of the dictyochophyte genus Pseudochattonella was observed in 1998, and since then such blooms have been observed in high cell densities in spring causing fish mortalities some years. Dinoflagellates, primarily Dinophysis spp., intermittently yield concentrations of Diarrhetic Shellfish Toxins (DST) in blue mussels, Mytilus edulis, above regulatory limits along the coasts of Norway, Denmark and the Swedish west coast. On average, DST levels in shellfish have decreased along the Swedish and Norwegian Skagerrak coasts since approximately 2006, coinciding with a decrease in the cell abundance of D. acuta. Among dinoflagellates, Alexandrium species are the major source of Paralytic Shellfish Toxins (PST) in the region. PST concentrations above regulatory levels were rare in the Skagerrak-Kattegat during the three decadal review period, but frequent and often abundant findings of Alexandrium resting cysts in surface sediments indicate a high potential risk for blooms. PST levels often above regulatory limits along the west coast of Norway are associated with A. catenella (ribotype Group 1) as the main toxin producer. Other Alexandrium species, such as A. ostenfeldii and A. minutum, are capable of producing PST among some populations but are usually not associated with PSP events in the region. The cell abundance of A. pseudogonyaulax, a producer of the ichthyotoxin goniodomin (GD),has increased in the Skagerrak-Kattegat since 2010, and may constitute an emerging threat. The dinoflagellate Azadinium spp. have been unequivocally linked to the presence of azaspiracid toxins (AZT) responsible for Azaspiracid Shellfish Poisoning (AZP) in northern Europe. These toxins were detected in bivalve shellfish at concentrations above regulatory limits for the first time in Norway in blue mussels in 2005 and in Sweden in blue mussels and oysters (Ostrea edulis and Crassostrea gigas) in 2018. Certain members of the diatom genus Pseudonitzschia produce the neurotoxin domoic acid and analogs known as Amnesic Shellfish Toxins (AST). Blooms of Pseudo-nitzschia were common in the North Sea and the Skagerrak-Kattegat, but levels of AST in bivalve shellfish were rarely above regulatory limits during the review period. Summer cyanobacteria blooms in the Baltic Sea are a concern mainly for tourism by causing massive fouling of bathing water and beaches. Some of the cyanobacteria produce toxins, e.g. Nodularia spumigena producer of nodularin, which may be a human health problem and cause occasional dog mortalities. Coastal and shelf sea regions in northern Europe provide a key supply of seafood, socioeconomic well-being and ecosystem services. Increasing anthropogenic influence and climate change create environmental stressors causing shifts in the biogeography and intensity of HABs. Continued monitoring of HAB and phycotoxins and the operation of historical databases such as HAEDAT provide not only an ongoing status report but also provide a way to interpret causes and mechanisms of HABs.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
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  • 5
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    Diversity and regional distribution of harmful algal events along the Atlantic margin of Europe (2021)
    Elsevier
    In:  EPIC3Harmful Algae, Elsevier, ISSN: 15689883
    Details
    Publication Date: 2023-03-13
    Description: The IOC-ICES-PICES Harmful Algal Event Database (HAEDAT) was used to describe the diversity and spatiotemporal distribution of harmful algal events along the Atlantic margin of Europe from 1987 - 2018. The majority of events recorded are caused by Diarrhetic Shellfish Toxins (DSTs). These events are recorded annually over a wide geographic area from southern Spain to northern Scotland and Iceland, and are responsible for annual closures of many shellfish harvesting areas. The dominant causative dinoflagellates, members of the morphospecies ‘Dinophysis acuminata complex’ and D. acuta, are common in the waters of the majority of countries affected. There are regional differences in the causative species associated with PST events; the coasts of Spain and Portugal with the dinoflagellates Alexandrium minutum and Gymnodinium catenatum, north west France/south west England/south Ireland with A. minutum, and Scotland/Faroe Islands/Iceland with A. catenella. This can influence the duration and spatial scale of PST events as well as the toxicity of shellfish. The diatom Pseudo-nitzschia australis is the most widespread Domoic Acid (DA) producer, with records coming from Spain, Portugal, France, Ireland and the UK. Amnesic Shellfish Toxins (ASTs) have caused prolonged closures for the scallop fishing industry due to the slow depuration rate of DA. Amendments to EU shellfish hygiene regulations introduced between 2002 and 2005 facilitated end-product testing and sale of adductor muscle. This reduced the impact of ASTs on the scallop fishing industry and thus the number of recorded HAEDAT events. Azaspiracids (AZAs) are the most recent toxin group responsible for events to be characterised in the ICES area. Events associated with AZAs have a discrete distribution with the majority recorded along the west coast of Ireland. Ciguatera Poisoning (CP) has been an emerging issue in the Canary Islands and Madeira since 2004. The majority of aquaculture and wild fish mortality events are associated with blooms of the dinoflagellate Karenia mikimotoi and raphidophyte Heterosigma akashiwo. Such fish killing events occur infrequently yet can cause significant mortalities. Interannual variability was observed in the annual number of HAEDAT areas with events associated with individual shellfish toxin groups. HABs represent a continued risk for the aquaculture industry along the Atlantic margin of Europe and along the Atlantic margin of Europe and should be accounted for when considering expansion of the industry or operational shifts to offshore areas.
    Repository Name: EPIC Alfred Wegener Institut
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  • 6
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    Forecasting strong aftershocks in earthquake clusters from northeastern Italy and western Slovenia (2021)
    Elsevier
    Details
    Publication Date: 2023-10-25
    Description: 42 pages
    Description: In this study, we propose an analysis of the earthquake clusters that occurred in North-Eastern Italy and western Slovenia from 1977 to today. Given a mainshock generating alarm in the population, we are interested in forecasting if a similar magnitude earthquake will follow. We classify the earthquake clusters associated with mainshocks of magnitude Mm into two classes: if the strongest aftershock has a magnitude 〉=Mm-1 (swarms or large aftershock seismic sequences) as type A, otherwise (smaller aftershocks seismic sequences) as type B. A large aftershock following a main shock can cause significant damages to already weakened buildings and infrastructures, so a timely advisory information to the civil protection is of great interest for effective decision-making. For the first time, we applied to a new catalogue a pattern recognition algorithm for cluster type forecasting that we developed for all Italy (Gentili and Di Giovambattista, 2017). Thanks to the lower completeness magnitude of the local OGS catalogue, compared to the national one, and to a new version of the algorithm, we were able to lower the threshold of the clusters mainshocks magnitude from 4.5 to 3.7. The method has been validated by rigorous statistical tests. We tested the algorithm on the 1976 highly destructive earthquake cluster (mainshock magnitude 6.5 - the strongest in the last 80 years in the region) and we retrospectively forecasted it as an A cluster. Successful results were obtained also on other three smaller earthquake clusters in 2019.
    Description: Published
    Description: 106483
    Description: 4T. Sismicità dell'Italia
    Description: 6T. Studi di pericolosità sismica e da maremoto
    Description: JCR Journal
    Keywords: Physics - Geophysics; Physics - Geophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 7
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    Characteristic periods of the paleosecular variation of the Earth's magnetic field during the Holocene from global paleoreconstructions (2021)
    Elsevier
    Details
    Publication Date: 2023-10-25
    Description: The knowledge of the secular variation of the geomagnetic field at different time scales is important to determine the mechanisms that maintain the geomagnetic field and can help to establish constraints in dynamo theories. We have focused our study on the secular variation at millennial and centennial time scale searching for characteristic periods during the last 10 kyr. The frequency study was performed using four recent updated global paleomagnetic field reconstructions (SHA.DIF.14k, CALS10k.2, BIGMUDI4k and SHAWQ2k) by applying three techniques commonly used in signal analysis: the Fourier transform, the Empirical Mode Decomposition, and the wavelet analysis. Short-term variability of the geomagnetic field energy shows recurrent periods of around 2000, 1000–1400, and 600–800 and 250–400 years. The characteristic time around 600–800 years is well determined in all paleomagnetic reconstructions and it is mostly related to the axial dipole and axial octupole terms, but also observable in the equatorial dipole. In addition to this period, longer characteristic times of around 1000–1400 years are found particularly in the equatorial dipole and quadrupole terms in SHA.DIF.14k, CALS10k.2 and BIGMUDI4k while the 2000 year period is only well determined in the total geomagnetic field energy of SHA.DIF.14k and CALS10k.2. The most detailed paleoreconstructions for younger times also detect shortest characteristic times of around 250–400 years. The long-term variation of the geomagnetic energy is only observable in the axial dipole. A characteristic period of around 7000 years in both SHA.DIF.14k and CALS10k.2 has been found. This long period is related to two decays in the dipole field and a period of increasing intensity. The oldest decay took place between 7000 BCE and 4500 BCE and the present decay that started around 100 BCE. We have modeled the 4500 BCE up to present variation as a combination of a continuous decay, representing the diffusion term of the geomagnetic field, and one pulse that reinforces the strength of the field. Results show a characteristic diffusion time of around 11,000–15,000 years, which is compatible with the diffusion times of the dipole field used in geodynamo theories.
    Description: Published
    Description: 106656
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 8
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    Local earthquake tomography of the Larderello-Travale geothermal field (2021)
    Elsevier
    Details
    Publication Date: 2023-10-25
    Description: The Larderello-Travale Geothermal Field in South-West Tuscany (Italy) is the oldest and among the most pro- ductive geothermal fields in the world. A new 3D model of seismic P-wave velocity (V P ) of the upper crust beneath the geothermal field is derived by inverting a set of highly consistent travel-times from local-earth- quakes. Results document a marked correlation of V P with previously described, high-reflectivity horizons. We also determined a low velocity body (V P ∼5 km s −1 ) culminating at depths of about 7 km, with estimated vo- lume of 35–40 km 3 . Such low velocities are consistent with a granite at temperatures above 700 °C, thus in a partially-molten status.
    Description: Published
    Description: 101731
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Keywords: 04.01
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 9
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    Liquefaction source layer for sand blows induced by the 2016 megathrust earthquake (Mw 7.8) in Ecuador (Boca de Briceño) (2021)
    Elsevier
    Details
    Publication Date: 2023-10-24
    Description: Numerous sand boils were generated in the alluvial plain at the mouth of the Rio Brice˜no valley (Ecuador) during the Mw 7.8 earthquake of April 2016. The area is characterized by a series of raised marine terraces formed as a consequence of the rapid tectonic coastal uplift during the Quaternary. Boreholes and geotechnical investigations were carried during post-earthquake surveys and for the purpose of mitigating the liquefaction effects. Five lithological units were identified at a site of embankment, which represented continental-marine and transitional sedimentation since the Last Glacial Maximum. A comprehensive study of texture and petrographic composition of sand boils has been performed and compared with sandy silts and silty sands of the buried sedimentary sequence in order to identify the source levels for liquefaction. The petrographic components, in particular the low content of bioclasts and carbonate fragments of the sand boils, allow to pinpoint a source layer made up of fine-grained silty sands located between 2 and 4.5 m depth (Unit 2) whereas the deeper marine sands, richer in bioclasts, were not involved. The results support the idea that earthquake-induced liquefaction phenomena are not restricted to clean sands and well-sorted deposits, but may affect sand layers with significant amount of nonplastic silt.
    Description: Published
    Description: 102737
    Description: 5T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Description: JCR Journal
    Keywords: Earthquake-induced liquefaction ; Sand blows ; Ecuadorian coast ; Sand composition ; Holocene depositional sequences ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 10
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    Evidence for a large-magnitude Holocene eruption of Mount Rittmann (Antarctica): A volcanological reconstruction using the marine tephra record (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: In Antarctica, the near-source exposures of volcanic eruption deposits are often limited as they are not well preserved in the dynamic glacial environment, thus making volcanological reconstructions of explosive eruptions extremely challenging. Fortunately, pyroclastic deposits from explosive eruptions are preserved in Southern Ocean sediments surrounding Antarctica, and the tephrostratigraphy of these sequences offers crucial volcanological information including the timing and tempo of past eruptions, their magnitude, and eruption dynamics. Here we report the results of a tephrostratigraphy and tephrochronology study focused on four sediment cores recovered from the Wood Bay area in the western Ross Sea, Antarctica. In all these sedimentary sequences, we found a well-stratified primary tephra of considerable thickness, up to 80 cm, hereafter named the Aviator Tephra (AVT). According to the characteristics of the tephra deposit and its distribution, the AVT was associated with an eruption of considerable intensity, potentially representing one of the largest Holocene eruptions recorded in Antarctica. Based on the major and trace element geochemistry and the mineral assemblage of the tephra, Mount Rittmann was identified as the source of the AVT. A Holocene age of ∼11 ka was determined by radiocarbon dating organic material within the sediments and 40Ar-39Ar dating of alkali-feldspar crystals included in the tephra. Eruption dynamics were initially dominated by hydromagmatic magma fragmentation conditions producing a sustained, relatively wet and ash-rich eruptive cloud. The eruption then evolved into a highly energetic, relatively dry magmatic Plinian eruption. The last phase was characterized by renewed efficient magma-water interaction and/or collapse of the eruptive column producing pyroclastic density currents and associated co-ignimbritic plumes. The distal tephra deposits might be linked to the widespread lag breccia layer previously identified on the rim of the Mount Rittmann caldera which share the same geochemical composition. Diatoms found in the sediments surrounding the AVT and the primary characteristics of the tephra indicate that the Wood Bay area was open sea at the time of the eruption, which is much earlier than previously thought. AVT is also an excellent tephrostratigraphic marker for the Wood Bay area, in the Ross Sea, and a useful marker for future synchronization of continental ice and marine archives in the region.
    Description: Published
    Description: 106629
    Description: 1V. Storia eruttiva
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: 5A. Ricerche polari e paleoclima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 11
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    PICOSS: Python Interface for the Classification of Seismic Signals (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: Over the last decade machine learning has become increasingly popular for the analysis and characterization of volcano-seismic data. One of the requirements for the application of machine learning methods to the problem of classifying seismic time series is the availability of a training dataset; that is a suite of reference signals, with known classification used for initial validation of the machine outcome. Here, we present PICOSS (Python Interface for the Classification of Seismic Signals), a modular data-curator platform for volcano-seismic data analysis, including detection, segmentation and classification. PICOSS has exportability and standardization at its core; users can select automatic or manual workflows to select and label seismic data from a comprehensive suite of tools, including deep neural networks. The modular implementation of PICOSS includes a portable and intuitive graphical user interface to facilitate essential data labelling tasks for large-scale volcano seismic studies.
    Description: Published
    Description: 104531
    Description: 8T. Sismologia in tempo reale
    Description: JCR Journal
    Keywords: Volcanoes ; Software ; Classification ; Segmentation ; Detection ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 12
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    Shear wave velocity and attenuation structure of Ischia island using broad band seismic noise records (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: In volcanic areas, accurate localization of earthquakes requires detailed velocity and, possibly, attenuation models, taking into account wide lithological variability and high geothermal gradients. Ischia island (Campania region, Italy) is a seismically-active volcano recently affected by a Mw 3.9 event (Casamicciola, August 21, 2017, 1 km depth). Due to the lack of a specific velocity model, the earthquakes occurred on the island were localized using the one developed for the nearby Campi Flegrei caldera. The aim of this work is the definition of a mean representative 1D shear-wave velocity (Vs) and attenuation (Q) model of the shallower crust (up to 2 km depth) of Ischia. Seismic noise array and spectral ratios techniques were applied to broad band seismic signals recorded by temporary and permanent networks updated after the August 2017 earthquake. The values of both shear-wave velocity (Vs) and quality factor (Q) are realistic, with Q values comparable with those obtained for Campi Flegrei and Stromboli volcanic areas. By taking into account stratigraphic information from deep wells and ultrasonic measurements of velocity on granite and trachytic lava samples, a geological interpretation of the resulting velocity model is provided. Such a model can have significant implications for understanding the dynamics of a volcano, mainly those leading to seismic activity.
    Description: Published
    Description: 106970
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Keywords: Ischia volcanic island ; Shear wave velocity model ; Seismic attenuation ; Seismic noise ; Velocity and Attenuation model
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 13
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    Studying postseismic deformation of the 2010–2011 Rigan earthquake sequence in SE Iran using geodetic data (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: In this paper, we study the spatial distribution and temporal evolution of the postseismic deformation of the 2010–2011 Rigan earthquake sequence which occurred at the southern termination of the East Lut fault system, southeast Iran. One-year GPS measurements after the Rigan earthquake sequence reveals right-lateral postseismic displacement along the East Chahqanbar fault and left-lateral postseismic displacement along the South Chahqanbar fault. To investigate the deformation variations in time and space, InSAR time-series of COSMO-SkyMed images is applied using the Small Baseline Subset algorithm. The results confirm a clear cumulative postseismic signal increasing to 8 mm during the first five months following the first mainshock in the direction of the coseismic displacement. The cumulative postseismic displacements are well correlated with the cumulative number of the aftershocks and their associated moment release. Considering this correlation and the observation of a sharp discontinuity along the coseismic fault in the displacement map, it is concluded that the after-slip mechanism is responsible for the observed postseismic deformation in the study region. This study is the first observation of a short-term postseismic motion in eastern Iran through geodetic data in contrast with long-lasting postseismic displacements following the earthquakes that occurred around Lut block. Modeling of the postseismic displacement results in a distributed slip pattern with a maximum slip of 0.8 m on the fault plane responsible for the 2010 Rigan coseismic deformation. This indicates that the postseismic deformation on barriers remained unbroken during the mainshock.
    Description: Published
    Description: 228630
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Rigan earthquake ; Postseismic deformation ; InSAR ; Lut block Southeastern Iran
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 14
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    Improvements of data analysis and self-consistent monitoring methods for the MEV telescope (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: The MEV project is running for a long-term muography measurement at the North-East crater of the Etna Volcano, after the successful conclusion of the test phase in July 2017. Two sets of data were already acquired during 2017, during the last months of the summer, and 2018. Data analysis is currently ongoing in order to extract a two-dimensional density map of the target from the measured muon flux. But before, a major improvement on data pre-processing was required. It regards in particular the algorithm for event reconstruction and filtering and the introduction of a method to extract the telescope efficiency from data themselves. The main steps of this pre-analysis and their application to the test data set is described in this paper.
    Description: Published
    Description: 162052
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 15
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    The SoilExp software: An open-source Graphical User Interface (GUI) for post-processing spatial and temporal soil surveys (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: Preliminary interpretation of geological processes during field measurement campaigns require fast data analysis to adapt ongoing target strategies. It is the case of soil investigations where coupling geochemical and geophysical records favors a better understanding of subsurface processes. This task requires (i) statistical analysis to identify areas of interest during spatial surveys and (ii) signal processing to analyze temporal series. Here we present SoilExp, an open-source Python-based Graphical User Interface (GUI) that permits to process spatial and temporal surveys of soil gases (e.g. soil CO2 flux) combined with common physical parameters (e.g. self-potential, temperature) that are synchronously recorded on the field. SoilExp mixes innovative algorithms with the more common tools used for the analysis of both spatial surveys or temporal series. It offers the possibility to display distribution plots, maps, comparative plots, spectra and spectrograms, as well as data statistical analysis, in order to deal efficiently with datasets acquired on the field. Field measurements performed at Stromboli (Italy) supports that such software solution facilitates a quick visualization of the data output and is a powerful tool on the geochemical and geophysical analysis.
    Description: Published
    Description: 104553
    Description: 4V. Processi pre-eruttivi
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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    Renewable energy, institutional stability, environment and economic growth nexus of D-8 countries (2021)
    Elsevier
    Details
    Publication Date: 2023-10-26
    Description: The anthropogenic impact of conventional energy sources encourages the utilization of revenable energy, as it has become a strategic commodity for economic growth. On the other hand, institutional stability is the prerequisite...
    Description: Published
    Description: 100484
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: Renewable energy ; Non-renewable energy ; Institutional quality ; Economic output ; Environment quality ; D-8 countries
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    Making time in 2020 (2021)
    Elsevier
    In:  EPIC3Political Geography, Elsevier, 84, pp. 102332-102332, ISSN: 0962-6298
    Details
    Publication Date: 2023-10-30
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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    A simplified mechanical model for explaining fast-rising jökulhlaups (2021)
    Elsevier
    Details
    Publication Date: 2023-10-13
    Description: The paper describes a simplified mathematical model aimed at fitting available hydrographs of floods from subglacial lakes reaching their peak almost linearly in time, the so-called fast-risingjökulhlaups. The simplifying idea is that the glacier can be treated as a block with fixed width, length and thickness, confining a subglacial lake with a constant cross-sectional area and variable level. We do not consider the role of heat transfer as suggested by many authors for fast-rising events. The model consists of two ordinary differential equations: conservation equation for the lake water and motion equation for the glacier. The glacier vertical movement is supposed to be governed by its own weight, the water pressure generated by the lake and by the forces acting on the lateral sides due to interaction between the glacier and the surroundings. The model has three free parameters and reproduces satisfactorily eight historical hydrographs observed originated by eight jökulhlaups in the Skaftá river (Iceland). These floods, of fast-rising type, are sourced from two ice cauldrons, the Eastern one being responsible of the largest floods (up to 3500 m^3/s). On average, the cauldrons drain almost every two years due to persistent geothermal activity beneath Vatnajökull glacier. This periodicity has a simple mathematical interpretation and is used to obtain another validation of the model.
    Description: Published
    Description: 100013
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: JCR Journal
    Keywords: Subglacial floods ; Subglacial lakes ; Jökulhlaups ; Mathematical modelling
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    From conversion to conservation to carbon: The changing policy discourse on mangrove governance and use in the Philippines (2021)
    Elsevier
    In:  EPIC3Journal of Rural Studies, Elsevier, 82, pp. 184-195, ISSN: 0743-0167
    Details
    Publication Date: 2024-02-07
    Description: The current focus on mangroves as key ecosystems in mitigating the impacts of climate change has largely neglected the livelihoods of coastal dwellers interacting with mangroves. This article provides a review of scholarly and policy attention paid to these social groups and their means of struggle. It argues that the latest dominant governance discourse tying mangroves to blue carbon signifies a departure from catering to coastal people's interests and rights in mangroves. We describe the evolving discourses that have shaped mangrove use and conservation in the Philippines since the 1970s. While the mid-century preoccupation with mangrove conversion to fish farms gradually gave way to the pursuit of community-based mangrove conservation in the late 1980s and 1990s, recent experiences suggest a comparably weakened focus towards recognizing local access and use patterns. We contend that the present blue carbon framing of mangroves, which harbours technocratic and financialized ideals of sustainability, poses a fundamental disadvantage to local users of mangroves. We conclude by reflecting on ways to redress this trend via a new framing of mangroves.
    Repository Name: EPIC Alfred Wegener Institut
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  • 20
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    Humanising agricultural extension: A review (2021)
    Elsevier
    In:  EPIC3World Development, Elsevier, 140, pp. 105337-105337, ISSN: 0305-750X
    Details
    Publication Date: 2024-02-07
    Description: Agricultural extension is booming. This interest is critical in the context of numerous pressing issues linked to agrarian change and rural development. Because of its importance, extension has attracted significant critique for its persistent exclusion of social and political factors. In this light, the history of extension can be thought of as a paradigm composed of approaches aimed at increasing agricultural production through the transfer of technologies from experts to farmers, and a series of criticisms of technology transfer as hampered by neglect of socio-political factors, a process labelled ‘rendering technical’. By reviewing criticisms of extension for its rendering of socio-political factors, we account for the rendering of power, place, and people. Equally important, we offer examples that consolidate critiques in order to open the possibility that humanized extension may more successfully support farmers. Our review is an effort to engage extensionists in order to speak about power to those who attempt to speak truth to power.
    Repository Name: EPIC Alfred Wegener Institut
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  • 21
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    Characterizing the multidimensionality of microplastics across environmental compartments (2021)
    Elsevier
    In:  EPIC3Water Research, Elsevier, 202, pp. 117429-117429, ISSN: 0043-1354
    Details
    Publication Date: 2024-03-04
    Description: Understanding the multidimensionality of microplastics is essential for a realistic assessment of the risks these particles pose to the environment and human health. Here, we capture size, shape, area, polymer, volume and mass characteristics of 〉60,000 individual microplastic particles as continuous distributions. Particles originate from samples taken from different aquatic compartments, including surface water and sediments from the marine and freshwater environment, waste water effluents, and freshwater organisms. Data were obtained using state-of-the-art FTIR-imaging, using the same automated imaging post-processing software. We introduce a workflow with two quality criteria that assure minimum data quality loss due to volumetric and filter area subsampling. We find that probability density functions (PDFs) for particle length follow power law distributions, with median slopes ranging from 2.2 for marine surface water to 3.1 for biota samples, and that these slopes were compartment-specific. Polymer-specific PDFs for particle length demonstrated significant differences in slopes among polymers, hinting at polymer specific sources, removal or fragmentation processes. Furthermore, we provide PDFs for particle width, width to length ratio, area, specific surface area, volume and mass distributions and propose how these can represent the full diversity of toxicologically relevant dose metrics required for the assessment of microplastic risks.
    Repository Name: EPIC Alfred Wegener Institut
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  • 22
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    Characterizing the physical properties of gelatin, a classic analog for the brittle elastic crust, insight from numerical modeling (2021)
    Elsevier
    Details
    Publication Date: 2023-10-31
    Description: Precise characterization of the mechanical properties of gelatin, a classic analog of the elastic crust, is necessary for scaling the mechanical models of the Earth's crust behavior in laboratory experiments. Here we reassess how to accurately calculate the Young modulus (E) of gelatin contained in experimental tanks. By means of dedicated analog experiments and finite element simulations, we estimate the bias introduced by using equations appro­ priate for a half-space to interpret the subsidence due to a cylindrical surface load applied on the gelatin. In the case of a standard experimental setup with gelatin adhering to the tank wall, we find E is overestimated by at least 5% for a box with lateral size smaller than 20 times the cylinder diameter. In addition, we deduce a correction factor to be applied when using an analytical formula. We confirm that measuring the shear velocity leads to accurate estimates for the rigidity of gelatin. We also propose a new method for in situ Young's modulus estimation, relying on the length of air-filled propagating crack. Indeed, for a given injected volume, this length depends only on the density contrast between air and gelatin and on the Young's modulus of the gelatin. The fracture toughness of the gelatin is estimated independently. Direct comparison between fracture toughness and Young's modulus shows that for a given Young's modulus, salted gelatin has a higher fracture toughness than unsalted gelatin.
    Description: Published
    Description: 228901
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
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    Morphological and multivariate statistical analysis of quaternary monogenetic vents in the Central Anatolian Volcanic Province (Turkey): Implications for the volcano-tectonic evolution (2021)
    Elsevier
    Details
    Publication Date: 2023-10-31
    Description: The interaction and competition between magmatic and tectonic processes mostly control the spatial distribution and morphology of monogenetic volcanoes. The Central Anatolian Volcanic Province, situated in a strike slip environment, provides a remarkable opportunity to understand this relationship. We defined six monogenetic clusters and analyzed 540 Quaternary monogenetic volcanoes in terms of morphological and spatial characteristics. There is no distinct correlation among the morphological parameters of scoria cones or lava domes, possibly owing to the various factors and the sporadic nature of magmatic activity in the region. Our detailed multivariate statistical and vent alignment analyses together with several implications in the literature reveal that the CAVP is a tectonically-controlled intraplate volcanic field, which is mostly driven by regional deformations. The presence of both clustered and non-clustered vent distributions and the petrological characteristics of the volcanics within the region indicates that the dikes are derived directly by the pre-existing melt-bearing heterogeneous mantle (i.e., Egrikuyu monogenetic field) or the independent and short-lived shallow or deep crustal magma reservoirs (i.e., Nevsehir-Acig & ouml;l volcanic field). The local changes in the stress regimes and crustal lithology result in variations of field shape, spatial vent distribution, and vent alignments throughout the region. The triggering mechanisms for the initiation of the Quaternary volcanism in the region can be the lithosphericscale Central Anatolian fault zone, here considered as an immature rift zone where Erciyes volcanic field is developed and behaves as a possible magmatic transfer zone. Tuz G & ouml;l & uuml; fault zone as a western border of the so-called rift basin in the region is mostly responsible for the crustal propagation of magma, and the kinematic changes along this fault zone (i.e., strike-slip to normal) mostly shaped the spatial vent distributions and alignments of the clusters in its close proximity (e.g., Hasandag-Kegiboyduran volcanic field).
    Description: Published
    Description: 107280
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Keywords: Self-similar clustering ; Monogenetic volcanism ; Crustal deformation ; Central Anatolian Volcanic Province ; Tectonics, Volcanology, Geodynamics
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    Complexity measures of geomagnetic indices in the last two solar cycles (2021)
    Elsevier
    Details
    Publication Date: 2023-10-31
    Description: The SYM-H and AE geomagnetic indices can be considered as proxies of the response of the Earth’s magnetosphere and ionosphere to solar magnetic activity. They indirectly monitor some electric current systems which flow in the ionosphere and magnetosphere whose dynamics are directly or indirectly related to the Sun– Earth interaction. Consequently, their temporal changes reflect processes occurring in the near-Earth space, which contribute differently to the overall magnetosphere–ionosphere dynamics. The aim of this work is to characterize the nature of these two geomagnetic indices by following a complex system approach and applying a novel formalism, e.g., the EMD-based dominant amplitude multifractal formalism (EMD-DAMF). A set of complexity measures, i.e., the Hurst exponent (H), the singularity width (𝛥𝛼) and the spectrum width (𝛥𝑓), is evaluated for both geomagnetic indices analyzing data recorded during the last two solar cycles. One of the most significant findings of this study is the absence of relevant differences between the two solar cycles in terms of complexity measures for both geomagnetic indices, suggesting that only the occurrence and the frequency of geomagnetic storms and substorms affect the Hurst exponent and the singularity widths of SYM-H and AE indices. Moreover, while the AE index complexity measures do not show a significant dependence on geomagnetic activity, the SYM-H index shows a reduction in its complexity features during the geomagnetic storms, manifesting a more persistent behavior and moving from a (mono)fractal-like to a multifractal-like behavior when passing from quiet to disturbed periods. Finally, our findings are consistent with previous works on the forecast horizon of the geomagnetic activity as well as on the relation between the high-latitude ionosphere and the low-latitude magnetosphere, thus confirming the importance of providing higher resolution measures for correctly dealing with several Space Weather phenomena.
    Description: Published
    Description: 105583
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
    Keywords: near-Earth electromagnetic environment ; Geomagnetic indices ; Hilbert-Huang trasform ; complexity measures ; space weather ; 04.05. Geomagnetism
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    Echo occurrence in the southern polar ionosphere for the SuperDARN Dome C East and Dome C North radars (2021)
    Elsevier
    Details
    Publication Date: 2023-10-31
    Description: In this paper, echo occurrence rates for the Dome C East (DCE) and the new Dome C North (DCN) radars are studied. We report the ionospheric and ground scatter echo occurrence rates for selected periods around equinoxes and solstices in the final part of the solar cycle XXIV. The occurrence maps built in Altitude Adjusted Corrected Geomagnetic latitude and Magnetic Local Time coordinates show peculiar patterns highly variable with season. The comparisons of the radar observations with the International Reference Ionosphere model electron density and with ray tracing simulations allow us to explain the major features of observed patterns in terms of electron density variations. The study shows the great potential of the DCE and DCN radar combination to the Super Dual Auroral Radar Network (SuperDARN) convection mapping in terms of monitoring key regions of the high-latitude ionosphere critical for understanding of the magnetospheric dynamics.
    Description: Published
    Description: 100684
    Description: 2A. Fisica dell'alta atmosfera
    Description: JCR Journal
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    Combined approach of poroelastic and earthquake nucleation applied to the reservoir-induced seismic activity in the Val d’Agri area, Italy (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: In this work, an approach is developed to study the seismicity associated with the impoundment and changes of a water reservoir (reservoir induced seismicity, RIS). The proposed methodology features a combination of a semi-analytical poroelastic model with an earthquake nucleation approach based on rate-and-state frictional law. The combined approach was applied to the case of the Pertusillo Lake, located in the Val d’Agri area (Italy), whose large seasonal water level changes are believed to induce protracted micro-seismicity (local magnitude ML 〈 3). Results show that the lake impoundment in 1962 could have produced up to 0.5 bar changes in Coulomb failure stress (DCFS), while the seasonal water level variation is responsible for variation up to 0.05 bar. Modeling results of the seismicity rates in 2001- 2014 show that the observed earthquakes are well correlated with the modeled DCFS. Finally, the reason that the seismicity is only observed at southwest of the Pertusillo Lake is provided, which is likely attributed to different rock lithologies and depletion caused by significant hydrocarbon exploitation in the northeastern sector of the lake.
    Description: Published
    Description: 802-810
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
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    Investigation of the Norcia basin (Central Italy) through ambient vibration measurements and geological surveys (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: During the 2016–2017, a seismic sequence struck the Central Italy, involving four regions (Umbria, Marche, Abruzzo and Lazio) and causing important damages and victims in inhabited areas such as Norcia and Amatrice towns. The strongest event of the seismic sequence was a Mw 6.5 event with epicenter at about 5 km far from the Norcia area, which is an intermontane basin prone to ground motion amplification. The historical town of Norcia and the surrounding hamlets were recently investigated by the microzonation activity, but information on the geometry and velocity are still partial considering the entire basin. Indeed, past studies aimed at reconstructing the elastic and geometrical properties focusing mainly on the northern part of the basin. Specifically in this paper, we integrated seismic and geological data to get a better knowledge of the properties of the Quaternary Norcia basin. A geological survey was carried out to provide a geological map and three geological cross-sections. We analyzed new seismic ambient vibrations data, collected by single-seismic stations, to infer the distribution of resonant frequency (f0) for the entire basin. We used passive arrays of seismic stations to better define the velocity profiles of the area. In the northern part of the basin, two 2D arrays with elliptical-like shapes were deployed showing strong discrepancies of the elastic soil properties in proximity of Norcia town. We found shear-wave velocities of the near-surface profile of about 300–400 and 500–800 m/s in presence of palustrine and alluvial fan deposits, respectively. Further, the values of f0 are abruptly varying from 0.5 Hz in the SW sector of Norcia village up to 2 Hz in its NE sector. Ambient vibration data reveal less pronounced variation of f0 in the southern part of the basin, with resonant values that are almost in the range 1–1.3 Hz. In the southern sector, a 1D array was arranged along a 5-km line and was analyzed by means of seismic noise cross-correlation analysis suggesting the presence of a deeper seismic contrast. The integration of geophysical and geological results has allowed to infer insights on the subsurface geometry of the basin.
    Description: Published
    Description: 105501
    Description: 5T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Description: JCR Journal
    Keywords: 04.02. Exploration geophysics ; 04.06. Seismology
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    Recent volcano-tectonic activity of the Ririba rift and the evolution of rifting in South Ethiopia (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: The relationships between volcanic activity and tectonics at the southernmost termination of the Main Ethiopian Rift (MER), East Africa, still represent a debated problem in the MER evolution. New constraints on the timing, evolution and characteristics of the poorly documented volcanic activity of the Dilo and Mega volcanic fields (VF), near the Kenya-Ethiopia border are here presented and discussed. The new data delineate the occurrence of two distinct groups of volcanic rocks: 1) Pliocene subalkaline basalts, observed only in the Dilo VF, forming a lava basement faulted during a significant rifting phase; 2)Quaternary alkaline basalts, occurring in the twovolcanic fields as pyroclastic products and lava flows issued frommonogenetic edifices and covering the rift-related faults. 40Ar/39Ar dating constrains the emplacement time of the large basal lava plateau to ~3.7 Ma, whereas the youngest volcanic activity characterising the twoareas dates back to 134 ka (Dilo VF) to as recent as the Holocene (Mega VF). Volcanic activity developed along tectonic lineaments independent from those of the rift. No direct relations are observed between the Pliocene, roughly N-S-trending major boundary faults of the Ririba rift and the NE-SW-oriented structural trend characteristic of the Quaternary volcanic activity. We speculate that this change in structural trend may be the expression of (1) inherited crustal structures affecting the distribution of the recent volcanic vents, and (2) a local stress field controlled by differences in crustal thickness, following a major episode of reorganization of extensional structures in the region due to rift propagation and abandonment
    Description: Published
    Description: 106989
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Volcano-tectonic activity ; Continental rifting ; Rift evolution ; Inherited fabrics ; 40Ar/39Ar dating ; South Ethiopia ; evolution of rifting in South Ethiopia
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    In soil radon anomalies and volcanic activity on Mt. Etna (Italy) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: We present here the first attempt to understand the fast dynamics of an active basaltic volcano, namely Mt. Etna using soil gas radon measured in some sites located in strategic places around the volcano. Data were measured continuously from July 2015 to February 2017 and the raw signals were treated in order to filter out all possible periodic components that are normally due to non-volcanic factors, applying a method that does not require acquisition of other parameters, which are not always available. The residual signals highlighted seven anomalous changes, with radon values reaching levels from 2 to 5 times higher than the normal background. In six out of seven cases, anomalies were almost contemporaneous in all or almost all of the sites, indicating a common source for the observed radon variations. The pattern of anomalies suggests a transient wave-like propagation in the space/time domain, compatible with pressure-induced displacement of the gas. The observed patterns are most probably caused by the rapid upward motion of gas-rich magma into the volcano conduits, as almost all anomalies precede or accompany major volcanic events. In some cases, an alternative explanation could be the strong and sudden strain releases through earthquakes swarms, with consequent variations in the permeability of rocks at a large scale, given the apparent correlation between those anomalies and intense seismicity.
    Description: Published
    Description: 106267
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: 04.08. Volcanology
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    Experimental and thermodynamic constraints on mineral equilibrium inpantelleritic magmas (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Crystallization experiments on two pantellerites from Pantelleria, Italy, provide new evidence for the relationships between mineral phases in pantelleritic rocks aswell as the influence of temperature and redox conditions on mineral assemblages. Experiments were performed at 1 kbar with temperature ranging between 750–900°C, and fluid saturation conditionswith XH2O (=H2O/H2O+CO2) between 0 and 1. Redox conditionswere fixed at, or slightly below, the FMQbuffer. Results showthat at temperature of 900 °C pantelleriticmagmas arewell above the liquidus regardless their water content; we also observed a decrease in liquidus temperature (800°C) with increasingly reducing conditions. Mineral assemblages of the natural rocks have been successfully reproduced, particularly the relationship between fayalite and aenigmatite, which appear to be strongly controlled by melt peralkalinity, temperature and redox conditions. This is the first time that fayalitic olivine have been synthetized in experimental studies on pantellerites, which was found to be stable only for temperatures ≥750°C while amphibole can be stable at temperatures as high as 800°C at high fF2. Experimental results have been compared with the composition of mineral phases as well as with the results obtained from mineral equilibrium, geothermometry, and oxygen barometry studies on pantelleritic lava and tuffs from Pantelleria (Italy), Eburru (Kenya) and Menengai (Kenya). Petrological characteristics appear similar at different locations worldwide, with typical assemblages of anorthoclase and sodian clinopyroxene with variable fayalite, aenigmatite, Fe-Ti oxides and amphibole.
    Description: Published
    Description: 105793
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Pantellerite, Mineral Equilibria, Experimental Petrolog, Peralkaline magmas ; 03.01. General
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  • 31
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    Ultra-depleted melt refertilization of mantle peridotites in a large intra-transform domain (Doldrums Fracture Zone; 7–8°N, Mid Atlantic Ridge) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: The Doldrums transform system offsets the Equatorial Mid Atlantic Ridge by ~630 km at 7–8° N. This transform system consists of four intra-transform spreading centers (ITRs) bounded by five transform faults. The northernmost ITR is linked to the MAR axis by a ~ 180 km-long transform. Here, during two R/V A. N. Strakhov expeditions (S06 and S09), mantle peridotites were dredged along the transverse and median ridge of the transform, across the western flank of the ITR valley. Residual harzburgites were mainly sampled along the northern Doldrums transform valley, whereas plagioclase-bearing peridotites showing evidence for melt-rock interaction characterize the ITR domain. Petrological and geochemical observations reinforced by geochemical modelling are used to define the behaviour of trace elements during melt extraction and melt-rock reaction in our rocks. Results suggest that residual peridotites derive from mantle rocks that have undergone a degree of partial melting up to 12%, with melting likely starting at the transition of garnet-spinel stability fields, whereas peridotites which suffered melt-rock reactions have been divided into two types: (i) pl-impregnated peridotites, formed by migration of melts at high porosity and high melt-rock ratio; and (ii) refertilized peridotites, generated at reduced porosity, when small fractions of the same percolating melt crystallized clinopyroxene and minor plagioclase. We suggest that the refertilizing agent was a melt highly depleted in incompatible trace elements, in turn produced by an ultra-depleted mantle source. This mantle experienced previous degrees of melt extraction at the ridge axis, before being transposed laterally along the transform where it melted a second time during the opening of the intra-transform spreading segment.
    Description: Published
    Description: 105698
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Description: JCR Journal
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    An integrated multi-proxy study of cyclic pelagic deposits from the north-western Tethys: The Campanian of the Postalm section (Gosau Group, Austria) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: The Upper Cretaceous Postalm section in the Northern Calcareous Alps (Austria) exposes pelagic depositsof the northwestern Tethys whose cyclostratigraphy and palaeoenvironments were examined in thisstudy.The section displays rhythmic deposits of Santonian to late Campanian age (Gosau Group). The San-tonian/Campanian transition is characterised by condensed greyish carbonates, while the younger de-posits are composed of reddish foraminiferal packstones displaying distinct limestone-marl alternations.A biostratigraphic framework based on planktonic foraminifera and calcareous nannofossils is supportedby carbon and strontium isotope stratigraphy as well as magnetostratigraphy. The carbon isotope dataallow to correlate the Postalm section to other Tethyan reference sites and to identifyd13C events, such asthe Late Campanian Event. Spectral analyses of three independently assessed proxies (d13C, Fe contentand the thickness of limestone/marl couplets) in the upper, continuously exposed section part identified17 to 18 405 ka cycles spanning the mid to upper Campanian (Contusotruncana plummeraetoGansserinagansseriZones or CC21/UC15c to CC23a/UC16 nannofossil zones).
    Description: Published
    Description: 104704
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
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    The structure of Mediterranean arcs: New insights from the Calabrian Arc subduction system (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: The formation of Cenozoic mountain belts in the Mediterranean realm was preceded by tens of millions of years of subduction, forming volcanic arcs, and frontal contractional systems. In addition, subduction usually involves slab rollback and formation of oceanic backarcs. Although such structure must have influenced the orogeny of Mediterranean mountain belts, no active analog has been mapped with modern crustal-scale seismic methods. Here, we study the entire Calabrian subduction system to map the structure resulting from Tethys lithosphere subduction and slab rollback, in a process that must be akin to that operating during a phase of the formation of the Mediterranean orogenic belts. We present a crustal-scale cross section of the entire Calabrian subduction system obtained from on- and off-shore wide-angle seismic data. The 2D P-wave velocity section shows spatially abrupt (〈5 km of profile distance) structural and petrological transitions from the Ionian sedimentary wedge and Calabrian arc, to the rifted NW Calabrian margin, where the Quaternary Aeolian arc is emplaced. The margin, then, transitions northwards into the Marsili backarc region, where exhumed mantle and localized volcanism occurred during its formation. This complex structure implies rapid temporal and spatial changes between magmatic and amagmatic processes, and between compressional and extensional regimes during the evolution of this subduction system. We find that some terranes involved in the Alpine orogeny share petrological and tectonic similarities with some domains of the Calabrian subduction system. Based on the results of this study we propose the Calabrian Arc system as an analog for the subduction structuration that preceded the formation of Alpine orogenic systems.
    Description: Published
    Description: 116480
    Description: 1T. Struttura della Terra
    Description: JCR Journal
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  • 34
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    Potential mass movements on the Palinuro volcanic chain (southern Tyrrhenian Sea, Italy) and consequent tsunami generation (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: The Palinuro volcanic chain (PVC) is located about 80 km offshore the Campania region (Italy) in the southern sector of the Tyrrhenian Sea. The chain consists of 15 volcanic edifices aligned in an E-W direction with two distinct major seamounts (Palinuro and Glabro). They cover a 90 km long and 20 kmwide area, with a present-day volume of 2700 km3. Palinuro volcanism emplaced between 0.8 and 0.3 Ma, although shallow seismicity and hydrothermalism indicate an ongoing volcanic activity. A geomorphological analysis of the volcanic chain and data from a multichannel seismic profile reveal large volumes of buried chaotic material suggesting gravity mass sliding from the volcano flanks and slide scars. A stability analysis of the Palinuro flanks has been carried out to determine the sectors potentially prone to sliding in case of shallow volcanic earthquakes. Landslides are simulated by adopting a scenario-based approach. Tsunamis induced by these mass movements and their propagation across the Tyrrhenian Sea are modeled. Results suggest that shallow earthquakes (M ~4.6–4.8) are able to destabilize the flanks of the volcanic chain generating slope failures. Sliding volumes in the order of 1.5 km3 and 2.4 km3 may induce waves as high as 1.5 and 6 m, respectively, along the peri-Tyrrhenian coast. Our results underline the need for further investigations on the stability of the submarine volcanoes of the Tyrrhenian basin. These volcanoes are still poorly known although their instability could trigger large tsunamis along the southern Italy coastal sectors. Our recommendation is that multiparamertic monitoring networks on PVC and periodic oceanic cruises should be put into action, and further that a systematic evaluation of the tsunami hazard related to possible sliding phenomena on the flanks of the Tyrrhenian seamounts should be performed
    Description: Published
    Description: 107025
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
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  • 35
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    Palaeoecology of Middle Triassic tetrapod ichnoassociations (middle Muschelkalk, NE Iberian Peninsula) and their implications for palaeobiogeography in the western Tethys region (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: Tetrapod ichnology is a powerful tool to reconstruct the faunal composition of Middle Triassic ecosystems. However, reconstructions based on a single palaeoenvironment provide an incomplete and impoverished picture of the actual palaeodiversity. In this paper, we analyse Middle Triassic tetrapod ichnoassociations from the detrital Muschelkalk facies of the Catalan Basin of northeast Spain, ranging from terrestrial to coastal settings. We identified two main tetrapod ichnoassociations, preserved in two different palaeoenvironments, comprising the following ichnogenera and morphotypes: Procolophonichnium, Chelonipus, Rhynchosauroides, Rotodactylus, Chirotherium, Isochirotherium, Sphingopus, and indeterminate chirotheriids. We also statistically analyse a database of all known Middle Triassic tetrapod footprint localities worldwide; this database includes, for each track locality, the precise age, the palaeoenvironment and the presence/absence of ichnotaxa. Our results on the composition of ichnofauna within the palaeoenvironments of the Catalan Basin are integrated into this database. This approach allows us to revisit the palaeoenvironmental bias linked to the marine transgression that affected the Western Tethys region. Tetrapod ichnoassociations reveal the following palaeoenvironmental patterns: (1) in coastal settings, ichnoassociations are Rhynchosauroides-dominated and diversity is relatively low; (2) in terrestrial settings and those with less marine influences, ichnoassociations are non-Rhynchosauroides-dominated, usually characterised by more abundant chirotheriid tracks and, generally, a higher track diversity. The correlation between tetrapod ichnoassociations and sedimentary facies reveals how palaeoenvironmental constraints influenced faunal assemblages, especially those of the Middle Triassic of the Western Tethys region. Ichnoassociations allow the ecological response of tetrapod faunas to the environmental changes to be inferred for this critical time interval. Marine transgressions strongly influenced tetrapod ecosystems: environmental conditions were key for the faunal recovery in the aftermath of the end-Permian extinction, with the settlement of the so-called modern faunas and the rise of the dinosaur lineage.
    Description: Published
    Description: 110204
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
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  • 36
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    Crystal-mush reactivation by magma recharge: Evidence from the Campanian Ignimbrite activity, Campi Flegrei volcanic field, Italy (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: Processes of crystal-mush remobilization bymaficmagma recharges are often related to the outpouring of large volumes of silicic melt during caldera-forming eruptions. This occurred for the Campanian Ignimbrite (CI) eruption (Campi Flegrei, Italy), which produced a voluminous trachy-phonolitic ignimbrite in southern-central Italy about 40 ka ago.We focussed on the proximal-CI deposits at San Martino that are composed of a main sequence of early-erupted, crystal-poor units and a late-erupted (post-caldera collapse) crystal-rich Upper Pumice Flow Unit (UPFU). Detailed micro-analytical geochemical data were performed on glasses and crystals of pyroclasts from these deposits and coupledwith Sr-Nd isotopic measurements on glasses. Results show that the CI eruption was fed by two distinctmelts for the early-erupted units and the late UPFU, respectively. The glasses of the early erupted units have negative Eu anomalies and show more evolved compositions and higher Nd isotope ratios than those of the UPFU, which have positive Eu/Eu*. The magmas of the early units formed the main volume of eruptiblemelt of the CI reservoir, and are interpreted as having been extracted from cumulate crystal-mush without a vertical geochemical gradient within the magma reservoir. The data indicate that the generation of the distinctive UPFU melts involved the injection of a new batch of mafic magma into the base of the CI reservoir. The mafic magma allowed heating and reactivation of the CI crystal-mush by melting of low-Or sanidines (+/− low-An plagioclases), leaving high-An plagioclases and high-Mg# clinopyroxenes as residual phases and a crystal-mush melt, made of 20% of the initial mush interstitial melt (with a composition similar to the early erupted units) and 80% of sanidine melt. When the mush crystallinity was sufficiently reduced, the mafic magma was able to penetrate into the reactivated crystal-mush, mixing with variable proportions of crystalmush melt and generating cooler hybrid melts, which underwent further crystallization of high-Or sanidine at variable degrees (10–25%). Finally, possibly a short time before the eruption, the UPFU magmas were able to mix and mingle with the crystal-poor eruptible melts still persisting in the CI reservoir at the time of UPFU emission. We suggest that the complex mechanisms described for themagma evolution feeding the CI eruption may occur whenever a crystal-mush is reactivated by new mafic magma inputs .
    Description: Published
    Description: 105780
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
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    iFit: A simple method for measuring volcanic SO2 without a measured Fraunhofer reference spectrum (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Accurate quantification of the emission rate of sulphur dioxide (SO 2 ) from volcanoes provides both insights into magmatic processes and a powerful monitoring tool for hazard mitigation. The primary method for measuring magmatic SO 2 is Differential Optical Absorption Spectroscopy (DOAS) of UV scattered sunlight spectra, in which a reference spectrum taken outside the plume is used to quantify the SO2 slant column density inside the plume. This can lead to problems if the reference spectrum is contaminated with SO2 as this will result in a systematic underestimation of the retrieved SO2 slant column density, and therefore emission rate. We present a new analysis method, named ―iFit‖, which retrieves the SO 2 slant column density from UV spectra by directly fitting the measured intensity spectrum at high spectral resolution (0.01 nm) using a literature solar reference spectrum and measured instrument characteristics. This eliminates the requirement for a measured reference spectrum, providing a ―point and shoot‖ method for quantifying SO 2 slant column densities. We show that iFit retrieves correct SO2 slant column densities in a series of test cases, finding agreement with existing methods. We propose that iFit is suitable for both traverse measurements and permanent scanning stations, and could be integrated into volcano monitoring networks at observatories. Finally, we provide an open source software implementation of iFit with a user friendly graphical interface to allow users to easily utilise iFit.
    Description: Published
    Description: 107000
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: JCR Journal
    Keywords: 04.08. Volcanology
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  • 38
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    Structural and tectono-stratigraphic review of the Sicilian orogen and new insights from analogue modeling (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the subduction of the Alpine Tethys and the later collision of drifted continental blocks against the African and Apulian paleomargins. From North to South, the Sicilian Fold-and-Thrust Belt (SFTB) is divided in four main tectono-stratigraphic domains: (1) the Calabro-Peloritani terrane, drifted from the European margin, (2) the remnants of the Alpine Tethys accretionary Wedge (ATW) related to the subduction of the Tethys, (3) the folded and thrusted platform (Panormide) and deep-water (Imerese-Sicanian) series of the offscrapped African margin, and (4) the African foreland (Hyblean). Unfortunately, scarce quality seismic lines and outcrops of key tectono-stratigraphic units make the structure and dynamic evolution of the central-eastern part of the SFTB controversial. First, this study outlines through a review of the tectono-stratigraphic evolution of the central-eastern sector of the Sicilian orogen, the major remaining issues concerning: (1) the occurrence of inferred Alpine Tethys units far from the region where the remnants of the ATW outcrop (Nebrodi Mountains); both, in a forearc position above the Peloritani block to the North and in an active foreland context along the present day southern front of the belt; and (2) the diverging tectonic styles, from stacked large-scale tectonic nappes to foreland imbricated thrust systems rooted into a main basal décollement. Secondly, new constraints are given using analogue modeling to test mechanically the hypothesized structural and tectono-stratigraphic evolution of the SFTB. The experiment simulates the orogenic evolution of the SFTB at crustal-scale, from the Oligocene Tethys subduction, to the Middle Miocene-Late Pliocene continental collision between the European and African paleomargins. The tectono-stratigraphic synthesis is used to model the first-order mechanical stratigraphy of the sedimentary units involved in the Sicilian belt, as well as the imprint of the African margin structural inheritance. The experiments succeed in reproducing the general structure and tectono-stratigraphic evolution of the SFTB. In particular, the models support field observations hypothesing a gravity-driven origin of the inferred Alpine Tethys units intercalated within the forearc and foreland syntectonic sedimentation. Moreover, the model testifies of the main tectonic steps that led to the SFTB building. First, a low-tapered accretionary wedge was accreted above the Alpine Tethys oceanic crust from the Oligocene to the Early Miocene. The following underthrusting of the stretched African continental margin and its frontal Panormide platform shortened and thickened the accretionary wedge. This phase provided favorable conditions for significant pulses of reworked Alpine Tethys units that intercalated within the forearc and foredeep successions. During the Middle-Miocene, the décollement of the African Meso-Cenozoic cover (Panormide platform and Imerese-Sicanian deep-water basin) enhanced a deep-seated deformation phase, along with duplexing of the Panormide platform beneath the Alpine Tethys wedge leading to its emersion. Since the Late Messinian, activation of basement faults led to a generalized emersion of the orogenic units through large-wavelength fold culminations accompanied by syntectonic deposition at their southern limbs. Concurrently, the prism front was partly indented to the southeast by the thick and locally already emerged Hyblean platform.
    Description: Published
    Description: 103257
    Description: 1T. Struttura della Terra
    Description: JCR Journal
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    Strombolian eruptions and dynamics of magma degassing at Yasur Volcano (Vanuatu) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: Open vent basaltic volcanoes account for a substantial portion of the global atmospheric outgassing flux, largely through passive degassing and mild explosive activity. We present volcanic gas flux and composition data from Yasur Volcano, Vanuatu collected in July 2018. The average volcanic plume chemistry is characterised by a mean molar CO2/SO2 ratio of 2.14, H2O/SO2 of 148 and SO2/HCl of 1.02. The measured mean SO2 flux in the period of 6th to 9th July is 4.9 kg s−1 . Therefore, the mean fluxes of the other species are 7.5 kg∙s −1 CO2, 208 kg∙s −1 H2O and 4.8 kg∙s −1 HCl. The degassing regime at Yasur volcano ranges from ‘passive’ to ‘active’ styles, with the latter including Strombolian activity and spattering. Gases emitted during active degassing are enriched in SO2 over HCl and CO2 over SO2 relative to passive degassing, with CO2/SO2 ratios of 2.85 ± 0.17, SO2/HCl of 1.6 ± 0.22, and H2O/SO2 of 315 ± 78.8. Gases emitted during passive degassing have CO2/SO2 ratios of 1.96 ± 0.12, SO2/ HCl of 0.50 ± 0.07 and H2O/SO2 of 174 ± 43.5. We use a model of volatile degassing derived from melt inclusion studies (Metrich et al., 2011), combined with our observations of chemical variations in the outgassing bubbles to propose a mechanism for magma degassing in the conduit at Yasur. We envisage a shallow conduit filled with crystal-rich magma, forming a viscous and mobile plug that develops an effective yield strength from the surface to a depth of at least 2000 m, in which bubbles are trapped, grow, ascend towards the surface and burst in a typical Strombolian eruption. Deeper bubbles released during active degassing are enriched in CO2 and SO2 compared to bubbles released during ‘passive degassing’, which are sourced from close to the surface, and are, consequently, HCl-rich.
    Description: Published
    Description: 106869
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
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  • 40
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    Plant root penetration and growth as a mechanical inclusion problem (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: The ability of plant roots to penetrate soils is affected by several stimuli exerted by the surrounding medium, such as mechanical stresses and chemical stimuli. Roots have developed different adaptive responses, such as increase or decrease of the elongation rate of the apical region and swelling or shrinking of its diameter. We propose a mathematical model aimed at explaining the dynamic evolution of plant roots during the penetration into the soil. We treat the root as a cylinder and the root–soil interaction as a purely mechanical inclusion problem. In particular, the root dynamic evolution is based on a modified version by one of the authors of the extended universal law of West, Brown, and Enquist. Coupling the solution of the mechanical problem and the growth equation, we compare the theoretical results with experimental data collected in artificial and real soils. In this work, we propose a plausible interpretation of the experimental results of the root behavior during the growth inside the surrounding soil medium.
    Description: Published
    Description: 103344
    Description: 7A. Geofisica per il monitoraggio ambientale
    Description: JCR Journal
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  • 41
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    Minor earthquake sequences in the Amatrice-Norcia epicentral area (Central Italy) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: This study presents a detailed analysis of minor seismic sequences recorded in the Amatrice-Norcia area (central Italy) before 2016 when the most important seismic sequence of the last 40 years struck the region with the Mw 6.0 Amatrice and the Mw 6.5 Norcia earthquakes. We observe that, in the four decades before the 2016–2018 Amatrice-Visso-Norcia sequence, the instrumental seismicity rate is low, with maximum magnitudes lower than Mw 4.0, and is characterized by different types of behaviours as single shock events, swarms and minor se- quences. For the first time, we relocate the minor seismicity recorded before 2016 by the Italian National Seismic Network of the Istituto Nazionale di Geofisica e Vulcanologia by applying the nonlinear inversion code Non- LinLoc in a local velocity model. Revised earthquake locations of the past seismic sequences are compared to the recent 2016–2018 seismicity in order to investigate some possible correlations with the seismogenic structures reactivated in 2016. With this goal, we also integrated our new hypocentral locations with fault plane solutions and geological data to interpret our results with respect to the 2016–2018 seismicity. Our results show how some of the structures identified by the minor seismicity before 2016 were reactivated during the recent sequence, while others seismic structures remained silent. We therefore highlight how the study of minor seismic sequences provides important information about the seismogenic attitude of less active or less known seismogenic struc- tures with consequent impact on the evaluation of the seismic hazard.
    Description: Published
    Description: 228858
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Keywords: 04.07. Tectonophysics ; 04. Solid Earth
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  • 42
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    The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: We present the first isotopic (noble gases and CO2) characterization of fluid inclusions coupled to Raman microspectroscopy analyses in mantle xenoliths from Central Mexico, a geodynamically complex area where the Basin and Range extension was superimposed on the Farallon subduction (terminated at 28 Ma). To characterize the isotopic signature of the Central Mexican lithospheric mantle, we focus on fluid inclusions entrapped in mantle xenoliths found in deposits of the Joya Honda maar (JH), a Quaternary monogenetic volcano belonging to the Ventura Espiritu Santo Volcanic Field (VESVF) in the state of San Luis Potosí (central Mexico). Thirteen ultramafic plagioclase-free xenoliths were selected, all exhibiting a paragenesis Ol 〉 Opx 〉 Cpx 〉 〉 Sp, and being classified as spinel-lherzolites and harzburgites. All xenoliths bring textural evidence of interstitial glass veins bearing dendritic trails of secondary melt and fluid inclusions (composed of silicate glass ± CO2 ± Mg-Ca carbonates ± pyrite). These are related to pervasive mantle metasomatism driven by carbonate-rich silicate melt. The Ar and Ne systematics reflect mixing between MORB-like upper mantle and atmospheric fluids, the latter interpreted as reflecting a recycled air component possibly inherited from the Farallon plate subduction. The 3He/4He ratios vary between 7.13 and 7.68 Ra, within the MORB range (7–9 Ra), and the 4He/40Ar* ratios (0.4–3.11) are similarly close to the expected range of the fertile mantle (1–5). Taken together, these pieces of evidence suggest that (i) either the mantle He budget was scarcely modified by the Farallon plate subduction, and/or (ii) that any (large) crustal contribution was masked by a later metasomatism/refertilization episode, possibly during the subsequent Basin and Range extension. A silicate melt-driven metasomatism/refertilization (revealed by the association between glass veins and fluid inclusions) is consistent with calculated helium residence time for the Mexican lithospheric mantle (20 to 60 Ma) that overlaps the timing of the above geodynamic events. We propose that, after the refertilization event (e.g., over the last ~20 Ma), the lithospheric mantle has evolved in a steady-state, becoming slightly more radiogenic. We also estimated 3He fluxes (0.027–0.080 mol/g), 4He production rates (340–1000 mol/yr), and mantle CO2 fluxes (3.93 × 107 mol/yr to 1.18 × 108 mol/yr) using the helium isotopic values measured in JH mantle xenoliths. Finally, the JH xenoliths exhibit CO2/3He ratios comparable to those of the upper mantle (from 3.38 × 108 to 3.82 × 109) but more positive δ13C values (between - 1.0 and - 2.7‰), supporting the involvement of a crustal carbonate component. We propose that the metasomatic silicate melts recycled a crustal carbonate component, inherited by the Farallon plate subduction.
    Description: Published
    Description: 120270
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Keywords: Mexican mantle xenoliths ; Fluid inclusions ; Noble gases ; CO2 ; mantle refertilization ; Carbonate recycling ; 04.01. Earth Interior ; 04.08. Volcanology
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  • 43
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    Tephrochronology of the central Mediterranean MIS 11c interglacial (∼425–395 ka): New constraints from the Vico volcano and Tiber delta, central Italy (2021)
    Elsevier
    Details
    Publication Date: 2023-11-14
    Description: Through a systematic integrated approach, which combined lithostratigraphic, geochronological and geochemical analyses of tephra from near-source sections of the peri-Tyrrhenian volcanoes and mid to distal settings, here we provide an improved tephrochronological framework for the Marine Isotope Stage 11c interglacial (MIS 11c, ~425e395 ka) in the Central Mediterranean area. Specifically, we present the complete geochemical dataset and new high-precision 40Ar/39Ar ages of the previously poorly characterized earliest pyroclastic products of the Vico volcano (420e400 ka), including the Plinian eruptions of Vico a and Vico b and the immediately post-dating lower magnitude explosive events. Furthermore, we also provide new geochronological and geochemical data for the distal tephra layers preserved in the aggradational succession of the Tiber delta (San Paolo Formation), Roman area, which records sea level rise relating to the MIS 12 (glacial) to MIS 11 (interglacial) transition. Five pyroclastic units were recognized in Vico volcanic area, four out of which, Vico a, Vico b, Vico btop (a minor eruption immediately following Vico b and temporally very close to it) and Vico d were directly dated at 414.8 ± 2.2 ka, 406.5 ± 2.4 ka, 406.4 ± 2.0 ka and 399.7 ± 3.2 ka respectively (2s analytical uncertainties). These new data allow a critical reappraisal of the previously claimed identifications of Vico tephra from mid-distal to ultra-distal successions (i.e., Vico-Sabatini volcanic districts, Roman San Paolo Formation and Castel di Guido archaeological site, Sulmona Basin, Valdarno and Lake Ohrid), which were unavoidably biased by the poor and incomplete geochemical and geochronological reference datasets previously available. Such an improvement of the tephrochronological framework brings great benefits to any future investigations (e.g., paleoclimatology, archaeology, active tectonic, volcanology) in the dispersal areas of the studied eruptions at the key point in time that is MIS 11.
    Description: Published
    Description: 106470
    Description: 1V. Storia eruttiva
    Description: JCR Journal
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  • 44
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    The case study of Case Bastione: First analyses of 3rd millennium cal BC paleoenvironmental and subsistence systems in central Sicily (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Archaeological investigations carried out at Case Bastione (Enna, central Sicily) provide a key insight into the cultural and environmental changes that occurred during the transition from the Copper Age to the Bronze Age. Preliminary data of an ongoing paleoenvironmental reconstruction through archaeobotanical analyses are here presented. The selective exploitation of vegetation, the adaptation of lifestyle to local resources, and changing climatic conditions are analysed using different on-site and off-site environmental and archaeological proxies. The environment around the site was constituted by mixed oak woodland. Dietary preferences were reconstructed through the analysis of carpo-remains. Isotopic values provide new data on the 4.2 ka BP event and its effects on vegetation in central Sicily. In a whole, first results from Case Bastione give new light to human choices of vegetal resources exploitation. Comparison of the local results with the regional pollen data support the hypothesis that the growth in population and settlement in the inland part of the island since the Late Copper Age may reflect changing climatic conditions in coastal areas.
    Description: Published
    Description: 102332
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
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    Recycled crustal carbon in the depleted mantle source of El Hierro volcano, Canary Islands (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: The Canary Islands, in the eastern Atlantic, are among the most enigmatic Oceanic Island provinces on Earth, as the mantle source feeding its volcanism exhibits wide spatial heterogeneity and a multiplicity of sources. Multiisotope whole-rock studies have long revealed the presence of a recycled oceanic crust/lithosphere component in the mantle source. However, noble gas systematics have been more challenging to interpret, and the available carbon isotope data is limited and cannot support/dismiss this interpretation. Here, we present the very first isotopic characterisation of CO2 and noble gases (He-Ne-Ar) in fluid inclusions (FI) in minerals hosted in mantle xenoliths from El Hierro, the youngest and westernmost island of the Canary volcanic archipelago. Six fresh xenoliths from El Julan cliff valley were analysed (3 spinel lherzolites and 3 spinel harzburgites). We find carbon isotopic compositions of CO2 in FI (δ13C) ranging from 􀀀 2.38 to 􀀀 1.23‰ in pyroxenes and from 􀀀 0.19 to +0.96‰ in olivines. These unusually positive δ13C values, well above the typical mantle range (􀀀 8‰ 〈 δ13C 〈 􀀀 4‰), prove, for the first time, the presence of a recycled crustal carbon component in the local source mantle. We interpret this 13C-rich component as inherited from a mantle metasomatism event driven by fluids carrying carbon from C. In contrast, our El Hierro xenoliths identify a depleted mantle-like He signature, with an average Rc/Ra ratio (3He/4He normalised to air ratio and corrected for atmospheric contamination) of 7.45 ± 0.26 Ra. The involvement of depleted mantle-like fluids, variably admixed with air-derived components (possibly recycled via paleo-subduction event(s)), is corroborated by Ne-Ar isotopic compositions. The depleted mantle-like He signature suggests instead the involvement of a primordial He source in the local lithospheric mantle and indicates a marginal role played by past subduction events in modifying the local mantle He budget. When put in the context of previous 3He/4He measurements in FI and surface gases along the Canary archipelago, our results confirm an overall west-to-east decrease of Rc/Ra ratios, which may be interpreted as due to increasing contributions from the African sub-continental mantle, the addition of radiogenic 4He during magma migration in the oceanic crust (whose thickness increases eastward) and/or magma ageing.
    Description: Published
    Description: 106414
    Description: 1V. Storia eruttiva
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Keywords: Canary Islands ; El Hierro ; Mantle xenoliths ; Fluid inclusions ; Recycled carbon ; noble gases ; 04.08. Volcanology ; 04.01. Earth Interior
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 46
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    Volcano dynamics vs tectonics on Mars: evidence from Pavonis Mons (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: Volcanic activity is widespread within the inner Solar system and it can be commonly observed on rocky planets. In this work, we analyse the structures of Pavonis Mons in the Tharsis volcanic province of Mars by performing structural mapping, azimuth, and topographic distribution of linear features on the flanks of Pavonis, such as grabens and pit chains. We tested whether their formation is to be ascribed to the volcano dynamics and magmatic activity or the tectonics. Through the length size distribution and fractal clustering analyses of the structural features, we found that large grabens are vertically confined in the upper mechanical layers of the brittle crust whereas pit chains penetrate the whole crust up to the magmatic source, indicating that they can be considered the main feeders of Pavonis Mons. We inverted the topography with dykes and faults models to test whether grabens at the surface are the expression of intrusions at depth and we suggest that thin dykes inducing normal faulting are the most likely mechanism. Furthermore, two azimuthal distribution of the grabens are identified: concentric grabens occur on the volcano summit while linear grabens at its base show NE-SW trend as the Tharsis Mons volcanos alignment. The occurrence of linear grabens suggests that Pavonis likely experienced a phase of active rifting with the formation of such structures, followed by a phase of volcano growth and concentric magma intrusions when volcano and magma chamber dynamics prevailed.
    Description: Published
    Description: 107148
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: JCR Journal
    Keywords: dykes and faults models ; rifting and volcano growth ; Pavonis Mons ; Mars ; Volcanology, Planetary Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 47
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    Investigating different vTEC calibration methods for data assimilation in ionospheric empirical models (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: A new data assimilation procedure in the International Reference Ionosphere UPdate (IRI UP) method has been recently implemented. This new procedure relies on the assimilation of vertical total electron content (vTEC) values from a Global Navigational Satellite Systems ground-based receivers network, calibrated through the Seemala’s method (IRI UP Seemala), to obtain an updated description of F2-peak ionospheric characteristics over the South-African region. The main purpose of this paper is to investigate how the use of different vTEC calibration methods affects the IRI UP method. In this work, the IRI UP method is applied on periods already analysed in the past (several quiet and disturbed periods in 2017 and 2018), but assimilating vTEC values calibrated through the Ciraolo’s method (IRI UP Ciraolo). In this way, it is possible to make a homogeneous and fair comparison between results obtained with the two different calibration methods. Overall, it emerges that IRI UP Ciraolo models foF2 with a precision that is always greater than the IRI UP Seemala’s one, mainly at nighttime and solar terminator hours, for both quiet and disturbed periods; while slight improvements are achieved during daytime hours. Their accuracy is instead quite similar. Anyhow, the IRI foF2 modeling over the South-African region is significantly improved by both procedures, thus providing a valuable tool to improve IRI model performances.
    Description: Published
    Description: 2138-2151
    Description: 2A. Fisica dell'alta atmosfera
    Description: 1IT. Reti di monitoraggio e sorveglianza
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 48
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    Mediterranean tephrostratigraphy and peri-Tyrrhenian explosive activity revaluated in light of the 430-365 ka record from Fucino Basin (central Italy) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Accurately reconstructing the scale and timing of dynamic processes, such as Middle-Late Pleistocene explosive volcanism and rapid climatic changes, requires rigorous and independent chronological constraints. In this framework, the study of distal volcanic ash layers, or tephra, transported and deposited over wide regions during explosive volcanic eruptions, is increasingly being recognised as a fundamental chronostratigraphic tool for addressing these challenging issues. Here we present a high-resolution distal tephra record preserved in the lacustrine sedimentary succession of the Fucino Basin, central Italy. The investigated record spans the 430-365 ka time interval, covering the entirety of Marine Isotope Stage 11 (MIS 11), and provides important insights into peri-Tyrrhenian potassic explosive volcanism from sources located in central Italy against a backdrop of Mediterranean palaeooclimate records. The succession of ash fall events of this time interval is reconstructed through a detailed lithostratigraphic, geochemical and 40Ar/39Ar geochronological characterization of the deposits preserved as discrete layers in the Fucino F4-F5 sediment core. This work is complemented by similarly detailed characterization of selected proximal pyroclastic units from the peri-Tyrrhenian potassic volcanoes. Geochemical fingerprinting of the tephra deposits by means of their major, minor and trace elements and Sr isotope composition indicates that all the thirty-two investigated ash layers derived from the peri-Tyrrhenian potassic volcanoes. The stratigraphically continuous succession of the Fucino tephra layers allowed the development of a fully independent, 40Ar/39Ar age-constrained, Bayesian age-depth model for the investigated time interval. The age-model allows us to establish modelled ages for the tephra layers within the succession that are not directly dated. The resulting dated tephra record clearly reveals a highly time resolved and previously unparalelled chronicle of explosive activity from the Vulsini, Vico, Sabatini, Colli Albani and Roccamonfina volcanic complexes. Our study provides a benchmark and valuable geochemical and geochronological dataset to be used as a reference for any future development and application of the tephrostratigraphic methods across the central Mediterranean area both during the investigated 430-365 ka time interval, and deeper in time. This contribution underlines the importance of integrating proximal and distal sedimentary records to more accurately establish long-term and comprehensive volcanic eruption records.
    Description: Published
    Description: 103706
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: Peri-Tyrrhenian explosive volcanism Mediterranean ; tephrochronology Marine ; tephrochronology Marine Isotope Stage 11
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 49
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    Kinetic partitioning of major and trace cations between clinopyroxene and phonotephritic melt under convective stirring conditions: New insights into clinopyroxene sector zoning and concentric zoning (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Within subvolcanic plumbing systems, along volcanic conduits and post-eruptive emplacement, mineral textures and compositions are governed by complex kinetic (undercooling) and dynamic (convective) processes that deviate from theoretical models and equilibrium criteria. In this perspective, we have investigated the partitioning of major and trace cations between clinopyroxene and phonotephritic melt under convective stirring conditions at high degrees of undercooling (−ΔTnominal = 30–60 °C) and atmospheric pressure. We have integrated this novel data set with conventional static (no physical perturbation) clinopyroxene-melt compositions obtained under interface- and diffusion-controlled growth regimes. Results show that clinopyroxene growth kinetics and diffusion boundary layers caused by melt supersaturation are partly mitigated by the homogenizing effects of stirring. Because of continuous supply of fresh melt to the advancing crystal surface, the partitioning of major and trace cations is governed by local equilibrium effects, which are interpreted as the extension of equilibrium thermodynamic principles to non-equilibrium bulk systems. Major cations are incorporated into the clinopyroxene structure via the coupled substitution [M1Mg, TSi] ↔ [M1Ti, TAl] and in conformity with the thermodynamic mixing properties of CaMgSiO2, CaAl2SiO6, and CaTiAl2O6 components. The complementary relationship between lattice strain (ΔGstrain) and electrostatic (ΔGelectrostatic) energies of heterovalent substitutions is the most appropriate thermodynamic description for the accommodation of trace cations in the clinopyroxene lattice site (i.e., ΔGpartitioning = ΔGstrain + ΔGelectrostatic). The excess energy of partitioning ΔGpartitioning changes principally with Al in tetrahedral coordination and determines the type and number of charge-balanced and -imbalanced configurations taking place in the structural sites of clinopyroxene. An important outcome from dynamic stirring experiments is that superimposition of convective mass transfer on melt supersaturation phenomena causes the formation of Cr-rich concentric zones under closed system crystallization conditions. However, these Cr-rich zones do not correlate with enrichment in other compatible elements and depletion in incompatible elements, as would be expected in natural open systems characterized by input of more primitive magmas. While the convective transport acts to reduce the diffusive length scale of chemical species in the experimental melt, fresh Cr cations are more easily incorporated into the concentric zones due to crystal field effects. Together, our findings reveal that during magma ascent and emplacement, convective stirring may promote clinopyroxene crystallization and minimize kinetic effects on clinopyroxene zoning.
    Description: Published
    Description: 120531
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 50
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    Multi-parametric characterization of explosive activity at Batu Tara Volcano (Flores Sea, Indonesia) (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: Batu Tara is an active but poorly studied volcano located in the Lesser Sunda Archipelago (Indonesia). Its last known long-lasting eruptive phase, dating 2006–2015, was characterised by frequent short-lived explosions, similar in style and magnitude to those of the well monitored Stromboli volcano (Italy). On September 2014, we collected high-frequency multi-parametric measurements of the ongoing explosive activity to investigate the dynamics of intermediate-size volcanic explosions. We acquired synchronized acoustic, thermal and visible high-speed imaging data, and parameterized different spatial and temporal properties of each explosive event: i) maximum height and ejection velocity of bombs and plumes, ii) duration, iii) amplitude of acoustic and thermal transients, iv) acoustic and thermal energy, v) spectral features of the acoustic signals. The latter ones justify the assumption of a pipe resonance of the uppermost conduit section, likely in response to the arrival of over-pressurized gas at the free magma surface. The variability of the investigated parameters agrees with previous observations of intermediate-size explosions at other volcanoes, reflecting the complexity of the related source processes.
    Description: Published
    Description: 107199
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 51
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    Parameterization of clinopyroxene growth kinetics via crystal size distribution (CSD) analysis: Insights into the temporal scales of magma dynamics at Mt. Etna volcano (2021)
    Elsevier
    Details
    Publication Date: 2023-11-16
    Description: There is increasing recognition that both textural and compositional changes of clinopyroxenes crystallizing from mafic alkaline magmas are the direct expression of complex dynamic processes extending over a broad range of spatial and temporal scales. Among others, supersaturation and relaxation phenomena play a key role in controlling the final crystal cargo of variably undercooled magmas erupted from active alkaline volcanoes. Following this line of reasoning, we have carried out isothermal- isobaric, decompression, and cooling rate experiments on a basalt interpreted as the parental magma of mafic alkaline eruptions at Mt. Etna volcano (Sicily, Italy). The main purpose is to reconstruct and quantify the textural changes (i.e., length of major and minor axes, surface area per unit volume, area fraction, and maximum growth rate) of clinopyroxene upon variable pressures (30-300 MPa), temperatures (1,050-1,100 °C), volatile contents (0-5 wt.% H 2 O and 0-0.2 wt.% CO 2 ), and equilibration times (0.25-72 h). By integrating experimental data and thermodynamic modeling, the transition between interface-controlled (euhedral morphologies) and diffusion- controlled (anhedral morphologies) growth regimes has been determined at an undercooling threshold value of ~33 °C. Early melt supersaturation causes the fast growth of tiny clinopyroxenes with strong disequilibrium shapes, whereas an increasing relaxation time leads to the slow growth of large clinopyroxenes showing textural equilibration. According to these kinetic principles, both growth rate and relaxation time have been parameterized in relation to the crystal size distribution (CSD) analysis of naturally undercooled clinopyroxenes erupted during 2011-2012 lava fountain episodes at Mt. Etna volcano. Results indicate that the crystallization of microlites and microphenocrysts takes place under (dis)equilibrium growth conditions, in the order of ~10 0 -10 1 min (large undercooling, short equilibration time) and ~10 1 -10 2 h (small undercooling, long equilibration time), respectively. This temporal information allows to disentangle the cooling and decompression paths of Etnean magmas rising and accelerating along a vertically extended, highly dynamic plumbing system. While clinopyroxene microlites develop during the fast ascent of magmas (~10 0 -10 1 m s -1 ) within the uppermost part of the conduit or immediately before ejection from the vent, the onset of microphenocryst crystallization occurs at depth and continues within the plumbing system during the slow ascent of magmas (~10 -2 m s -1 ) that migrate through interconnected storage regions.
    Description: Published
    Description: 106225
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 52
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    Deciphering a mantle degassing transect related with India-Asia continental convergence from the perspective of volatile origin and outgassing (2021)
    Elsevier
    Details
    Publication Date: 2023-11-21
    Description: Mantle degassing transect across different tectonic units within a plate convergent setting has been well documented for oceanic convergent margins by systematic changes in geochemistry (e.g., 3He/4He, d13C, and CO2/3He) of hydrothermal gases. However, little is known about spatial variations in volatile geochemistry across a continental convergent margin. In this study, we identify a mantle degassing transect in the southeastern Tibetan Plateau using He-CO2 systematics of hydrothermal gases, which extends from India-Asia continental convergent margin to intra-continent extensional region. d13C-CO2 ( 11.8‰ to 3.1‰) and CO2/3He (1.7 108 to 7.1 1011) values of hydrothermal gases show large variations that are consistent with modification by secondary physico-chemical processes, such as multi-component mixing, hydrothermal degassing, and calcite precipitation. Three levels of He degassing can be recognized based on 3He/4He dataset (0.01–5.87 RA) of the hydrothermal gas samples and their distances to volcanic centers. A magmatic level He degassing (35–74% mantle He) is found near active and/or Quaternary volcanoes fed by mantle-derived magmas. With increasing distance to volcanic centers, the outgassed magmatic volatiles are gradually diluted by crustal components (e.g., radiogenic 4He), defining a transitional level He degassing (13–33% mantle He). The 3He/4He values (8.16–8.48 RA) of olivine phenocrysts indicate a MORB (mid-ocean ridge basalts)-type mantle source for the magmatic and transitional levels of He degassing that are localized in Quaternary volcanic fields. In contrast, a background level He degassing (〈12% mantle He) dominates the entire study area, and can be attributed to (i) degassing of sub-continental lithospheric mantle, and/or (ii) higher degrees of crustal contamination than those of the transitional level He degassing near volcanic centers. Combined with olivine 3He/4He data reported in this study and whole-rock 87Sr/86Sr data of host basalts from literature, source components of the mantle-derived magmas are suggested to include the MORB-type convective mantle, subducted Indian slab materials, and less degassed mantle materials, which can account for the possible decoupling between He and Sr isotope systematics. These findings delineate the origin and outgassing of mantle volatiles controlled by the India-Asia continental convergence, and would contribute to a better understanding of the deeply-sourced volatile emissions in these tectonic settings.
    Description: Published
    Description: 61-78
    Description: 9T. Geochimica dei fluidi applicata allo studio e al monitoraggio di aree sismiche
    Description: JCR Journal
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  • 53
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    Erratum to “Permafrost degradation in a warmer Earth: Challenges and perspectives”, [Curr Opin Environ Sci Health, Volume 5, October 2018, Pages 14–18] (2021)
    Elsevier
    In:  EPIC3Current Opinion in Environmental Science & Health, Elsevier, 20, pp. 100231-100231, ISSN: 2468-5844
    Details
    Publication Date: 2024-04-19
    Description: Declaration of interest was missed out in the published version. The authors have confirmed in the following context: ‘The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.’ The publisher would like to apologise for any inconvenience caused.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev
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  • 54
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    Guanidinium Toxins: Evolution, Mode of Action and Chemical Ecology (2021)
    Elsevier
    In:  EPIC3Elsevier, ISBN: 9780128220146
    Details
    Publication Date: 2024-05-07
    Description: Marine Neurotoxins, Volume Five provides comprehensive information on marine toxins present in the human food chain and the affecting targets relevant for the functioning of the brain and our nervous system, covering all the information ...
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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  • 55
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    Spatiotemporal patterns of northern lake formation since the Last Glacial Maximum (2021)
    Elsevier
    In:  EPIC3Quaternary Science Reviews, Elsevier, 253, pp. 106773-106773, ISSN: 0277-3791
    Details
    Publication Date: 2024-01-30
    Description: The northern mid- to high-latitudes have the highest total number and area of lakes on Earth. Lake origins in these regions are diverse, but to a large extent coupled to glacial, permafrost, and peatland histories. The synthesis of 1207 northern lake initiation records presented here provides an analog for rapid landscape-level change in response to climate warming, and its subsequent attenuation by physical and biological feedback mechanisms. Our compilation reveals two peaks in northern lake formation, 13,200 and 10,400 years ago, both following rapid increases in North Atlantic air temperature. Placing our findings within the context of existing paleoenvironmental records, we suggest that solar insolationdriven changes in climate (temperature and water balance) that led to deglaciation and permafrost thaw likely contributed to high rates of northern lake formation during the last Deglacial period. However, further landscape development and stabilization dramatically reduced rates of lake formation beginning ~10,000 years ago. This suggests that temperature alone may not control future lake development; rather, multiple factors must align to enable a landscape to respond with an increase in lake area. We propose that land surfaces strongly geared toward increased lake formation were highly conditioned by glaciation. Thus, it is unlikely that warming this century will cause lake formation as rapid or as widespread as that during the last Deglacial period.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
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  • 56
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    The role of wetland expansion and successional processes in methane emissions from northern wetlands during the Holocene (2021)
    Elsevier
    In:  EPIC3Quaternary Science Reviews, Elsevier, 257(106864), ISSN: 0277-3791
    Details
    Publication Date: 2024-01-30
    Description: The contribution from northern high latitude wetlands are a major uncertainty in the atmospheric methane (CH4) budget throughout the Holocene. We reconstructed CH4 emissions from northern peatlands from 13,000 BP to present using an empirical model based on observations of peat initiation (〉3600 dates), peatland type (〉250 peat cores), and observed CH4 emissions in order to explore the effects of changes in wetland type on CH4 emissions over the end of the late glacial and the Holocene. Fen area increased steadily before 8000 BP as fens formed in major wetland complexes. After 8000 BP, new fen formation continued but widespread peatland succession (to bogs) and permafrost aggradation occurred. Reconstructed CH4 emissions from peatlands increased rapidly between 10,600 BP and 6900 BP due to fen formation and expansion. Emissions stabilized after 5000 BP at 42 ± 25 Tg CH4 y-1 as high-emitting fens transitioned to lower-emitting bogs and permafrost peatlands. Widespread permafrost formation in northern peatlands after 1000 BP decreased CH4 emissions by 20% to 34 ± 21 Tg y-1 by the present day and suggests peatland CH4 emissions will increase with permafrost thaw.
    Repository Name: EPIC Alfred Wegener Institut
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  • 57
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    The Arctic Nearshore Turbidity Algorithm (ANTA) - A multi sensor turbidity algorithm for Arctic nearshore environments (2021)
    Elsevier
    In:  EPIC3Science of Remote Sensing, Elsevier, 100036
    Details
    Publication Date: 2024-05-22
    Description: The Arctic is greatly impacted by climate change. The increase in air temperature drives the thawing of permafrost and an increase in coastal erosion and river discharge. This leads to a greater input of sediment and organic matter into coastal waters, which substantially impacts the ecosystems by reducing light transmission through the water column and altering the biogeochemistry, but also the subsistence economy of local people, and changes in climate because of the transformation of organic matter into greenhouse gases. Yet, the quantification of suspended sediment in Arctic coastal and nearshore waters remains unsatisfactory due to the absence of dedicated algorithms to resolve the high loads occurring in the close vicinity of the shoreline. In this study we present the Arctic Nearshore Turbidity Algorithm (ANTA), the first reflectance-turbidity relationship specifically targeted towards Arctic nearshore waters that is tuned with in-situ measurements from the nearshore waters of Herschel Island Qikiqtaruk in the western Canadian Arctic. A semi-empirical model was calibrated for several relevant sensors in ocean color remote sensing, including MODIS, Sentinel 3 (OLCI), Landsat 8 (OLI), and Sentinel 2 (MSI), as well as the older Landsat sensors TM and ETM+. The ANTA performed better with Landsat 8 than with Sentinel 2 and Sentinel 3. The application of the ANTA to Sentinel 2 imagery that matches in-situ turbidity samples taken in Adventfjorden, Svalbard, shows transferability to nearshore areas beyond Herschel Island Qikiqtaruk.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev , info:eu-repo/semantics/article
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  • 58
    Electronic Resource
    Electronic Resource
    A measurement of τ polarization in Z^0 decays (1992-8977)
    Amsterdam : Elsevier
    Physics Letters B 294 (1992), S. 466-478 
    Details
    ISSN: 0370-2693
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0370-2693(92)91549-O
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  • 59
    Electronic Resource
    Electronic Resource
    Measurement of the average lifetime of b hadrons (1993-4325)
    Amsterdam : Elsevier
    Physics Letters B 317 (1993), S. 474-484 
    Details
    ISSN: 0370-2693
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0370-2693(93)91027-K
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  • 60
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    Organic matter characteristics using lipid biomarker analysis of a rapidly eroding permafrost cliff (2021)
    PANGAEA
    Details
    Publication Date: 2023-01-27
    Description: Organic carbon (OC) stored in Arctic permafrost represents one of Earth's largest and most vulnerable terrestrial carbon pools. Amplified climate warming across the Arctic results in widespread permafrost thaw. Permafrost deposits exposed at river cliffs and coasts are particularly susceptible to thawing processes. Accelerating erosion of terrestrial permafrost along shorelines leads to increased transfer of organic matter (OM) to nearshore waters. However, the amount of terrestrial permafrost carbon and nitrogen as well as the OM quality in these deposits are still poorly quantified. Here, we characterise the sources and the quality of OM supplied to the Lena River at a rapidly eroding permafrost river shoreline cliff in the eastern part of the delta (Sobo-Sise Island). Our multi-proxy approach captures bulk elemental, molecular geochemical and carbon isotopic analyses of late Pleistocene Yedoma permafrost and Holocene cover deposits, discontinuously spanning the last ~52 ka. We show that the ancient permafrost exposed in the Sobo-Sise cliff has a high organic carbon content (mean of about 5 wt%).We found that the OM quality, which we define as the intrinsic potential to further transformation, decomposition, and mineralization, is also high as inferred by the lipid biomarker inventory. The oldest sediments stem from Marine Isotope Stage (MIS) 3 interstadial deposits (dated to 52 to 28 cal kyr BP) and is overlaid by Last Glacial MIS 2 (dated to 28 to 15 cal ka BP) and Holocene MIS 1 (dated to 7–0 cal ka BP) deposits. The relatively high average chain length (ACL) index of n-alkanes along the cliff profile indicates a predominant contribution of vascular plants to the OM composition. The elevated ratio of iso and anteiso-branched FAs relative to long chain (C ≥ 20) n-FAs in the interstadial MIS 3 and the interglacial MIS 1 deposits, suggests stronger microbial activity and consequently higher input of bacterial biomass during these climatically warmer periods. The overall high carbon preference index (CPI) and higher plant fatty acid (HPFA) values as well as high C / N ratios point to a good quality of the preserved OM and thus to a high potential of the OM for decomposition upon thaw. A decrease of HPFA values downwards along the profile probably indicates a relatively stronger OM decomposition in the oldest (MIS 3) deposits of the cliff.
    Language: English
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    REVEALS reconstruction of past vegetation cover, modern pollen and current vegetation data from Namibia (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Description: Understanding the resilience of African savannas to global change requires quantitative information on long-term vegetation dynamics. Here we present a reconstruction of past vegetation cover of the northern Namibian savanna obtained after applying the REVEALS model to fossil pollen data from Lake Otjikoto. We also present modern pollen and vegetation data used to calculate pollen productivity estimates for the major Namibian savanna taxa Acacia (Senegalia, Vachellia), Combretaceae, Dichrostachys, Grewia and Poaceae. Data were collected at 10 sites along a rainfall gradient in north central Namibia. Modern pollen was extracted from soil samples collected from plots at the different sites. Vegetation data were extracted from satellite images covering a 1.5 km radius from the plots where pollen was collected. The mean cover of the studied taxa was calculated by 100 m rings.
    Keywords: AWI_Envi; modern pollen; Polar Terrestrial Environmental Systems @ AWI; Pollen productivity estimate; REVEALS; Vegetation Mapping
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  • 62
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    High-resolution biomarker isotope and geochemical data for the ~4.2 ka sediment core from Lake Khar Nuur, Mongolian Altai (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-17
    Description: The Late Holocene is a substantial cultural and economic transition in the eastern Eurasian Steppe and Altai Region, but paleoclimate conditions during this time remain unclear. Therefore, we established a high-resolution paleoclimate record from Lake Khar Nuur in the Mongolian Altai, spanning the last 4200 years. Lake Khar Nuur is a high-altitude lake with a small catchment located at 2,486 m a.s.l. (48°37'22.9"N, 88°56'42.5"E). We recovered the sediment core (that we abbreviate KN18) from the deepest part of the lake (49.4 m) in July 2018 using an Uwitec gravity corer. Within the sediment core KN18, a wide array of lake sediment proxies was measured. While total organic carbon (TOC), total nitrogen, bulk δ^13^C~TOC~, δ^15^N and biogenic silica were measured in 2 cm resolution, the elemental composition (log (Ca/Ti) ratio) was measured in 0.5 cm resolution. Additionally, compound-specific hydrogen isotopic composition of _n_-alkanes was measured in 1 cm resolution.
    Keywords: Altai region; compound-specific biomarker isotopes; lake sediments; Late Holocene; Paleoclimate
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 63
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    Seasonal diel pH, dissolved inorganic carbon, total alkalinity and partial pressure of CO2 data in the seagrass meadows of the inner lagoon and northern shore of Dongsha Island during the 2016–2019 study period (Table 3) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CO2; DATE/TIME; Dongsha_Island_IL; Dongsha_Island_NS; Dongsha Island; Dongsha Island, China; Event label; IL; NS; Ocean acidification; pH; Seagrass
    Type: Dataset
    Format: text/tab-separated-values, 696 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 64
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    Soil properties considering pH-values, total nitrogen and carbon content of soil samples, and soil type determination based on sand, silt, clay composition at the Hordorf (Central Germany) groundtruthing sites (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: The data set contains the results of laboratory examination of 13 soil samples taken at the ground truthing reference sites during the flight campaign.
    Keywords: airborne; Clay; drought; evapotranspiration; Event label; Groundtruthing; HAND; heatwave; Modular Observation Solutions for Earth Systems; MOSES; MOSES_beets; MOSES_CV01; MOSES_CV02; MOSES_DIAG_00-99; MOSES_early_potatoes_B; MOSES_Kartoffel; MOSES_Kartoffel_frueh; MOSES_potatoes_A; MOSES_REF_Boden; MOSES_Ruebe; MOSES_S02; MOSES_S04; MOSES_S05; MOSES_S06; MOSES_S09; MOSES_S10; MOSES_soil_reference_site; Nitrogen, soil; Organic carbon, soil; pH; remote sensing; Sample ID; Sampling by hand; Sand; Silt; Site; Soil Moisture; soil properties; Soil type
    Type: Dataset
    Format: text/tab-separated-values, 117 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 65
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    Trait measurements of Sphagnum moss from northern peatlands (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: B1; B2; B3; B4; B5; B6; B7; B8; bog; Capitulum, dry weight; Capitulum, water content; Capitulum, width; Capitulum density; Carbon; Carbon/Nitrogen ratio; Elemental analyzer CHNS-O (EA1110); Elevation of event; Event label; Fascicle density; fen; functional plant trait; HL_HRS; HL_IS; HL_KAL; HL_KLA; HL_KS; HL_LA; HL_TE; Latitude of event; Longitude of event; Mire; mire succession; Moisture index; Nitrogen; Northern_peatlands_B1; Northern_peatlands_B2; Northern_peatlands_B3; Northern_peatlands_B4; Northern_peatlands_B5; Northern_peatlands_B6; Northern_peatlands_B7; Northern_peatlands_B8; Northern_peatlands_HL_HRS; Northern_peatlands_HL_IS; Northern_peatlands_HL_KAL; Northern_peatlands_HL_KLA; Northern_peatlands_HL_KS; Northern_peatlands_HL_LA; Northern_peatlands_HL_TE; Northern_peatlands_S1; Northern_peatlands_S13; Northern_peatlands_S2; Northern_peatlands_S3; Northern_peatlands_S31; Northern_peatlands_S33; Northern_peatlands_S4; Northern_peatlands_S41; Northern_peatlands_S42; Northern_peatlands_S5; Northern_peatlands_S51; Northern_peatlands_S53; Northern_peatlands_S6; Northern_peatlands_u10; Northern_peatlands_u13; Northern_peatlands_u14; Northern_peatlands_u16; Northern_peatlands_u18; Northern_peatlands_u2; Northern_peatlands_u24; Northern_peatlands_u26; Northern_peatlands_u29; Northern_peatlands_u33; Northern_peatlands_u43; Northern_peatlands_u52; Northern_peatlands_u62; Northern_peatlands_u65; Northern_peatlands_u70; Optional event label; Peatland; Peat thickness; pH; S1; S13; S2; S3; S31; S33; S4; S41; S42; S5; S51; S53; S6; Species; u10; u13; u14; u16; u18; u2; u24; u26; u29; u33; u43; u52; u62; u65; u70
    Type: Dataset
    Format: text/tab-separated-values, 4199 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 66
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    Vascular trait measurements from northern peatlands (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: B1; B2; B3; B4; B5; B6; B7; B8; bog; Carbon; Carbon/Nitrogen ratio; Elemental analyzer CHNS-O (EA1110); Elevation of event; Event label; fen; functional plant trait; HL_HRS; HL_IS; HL_KAL; HL_KLA; HL_KS; HL_LA; HL_TE; Latitude of event; Leave size; Longitude of event; Measured using software ImageJ; Mire; mire succession; Moisture index; Nitrogen; Northern_peatlands_B1; Northern_peatlands_B2; Northern_peatlands_B3; Northern_peatlands_B4; Northern_peatlands_B5; Northern_peatlands_B6; Northern_peatlands_B7; Northern_peatlands_B8; Northern_peatlands_HL_HRS; Northern_peatlands_HL_IS; Northern_peatlands_HL_KAL; Northern_peatlands_HL_KLA; Northern_peatlands_HL_KS; Northern_peatlands_HL_LA; Northern_peatlands_HL_TE; Northern_peatlands_S1; Northern_peatlands_S11; Northern_peatlands_S2; Northern_peatlands_S3; Northern_peatlands_S31; Northern_peatlands_S33; Northern_peatlands_S4; Northern_peatlands_S41; Northern_peatlands_S42; Northern_peatlands_S5; Northern_peatlands_S51; Northern_peatlands_S53; Northern_peatlands_S6; Northern_peatlands_u10; Northern_peatlands_u13; Northern_peatlands_u14; Northern_peatlands_u16; Northern_peatlands_u18; Northern_peatlands_u2; Northern_peatlands_u24; Northern_peatlands_u26; Northern_peatlands_u29; Northern_peatlands_u33; Northern_peatlands_u43; Northern_peatlands_u52; Northern_peatlands_u62; Northern_peatlands_u65; Northern_peatlands_u70; Optional event label; Peatland; Peat thickness; pH; Plant height; S1; S11; S2; S3; S31; S33; S4; S41; S42; S5; S51; S53; S6; Species; Specific leaf area; u10; u13; u14; u16; u18; u2; u24; u26; u29; u33; u43; u52; u62; u65; u70
    Type: Dataset
    Format: text/tab-separated-values, 19294 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 67
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    Fractional abundances and concentrations of brGMGTs in SPM from Lake Chala (Table S1) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Africa; Branched glycerol monoalkyl glycerol tetraethers; Branched glycerol monoalkyl glycerol tetraethers, H1020a; Branched glycerol monoalkyl glycerol tetraethers, H1020a, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1020b; Branched glycerol monoalkyl glycerol tetraethers, H1020b, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1020c; Branched glycerol monoalkyl glycerol tetraethers, H1020c, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1034a; Branched glycerol monoalkyl glycerol tetraethers, H1034a, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1034b; Branched glycerol monoalkyl glycerol tetraethers, H1034b, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1034c; Branched glycerol monoalkyl glycerol tetraethers, H1034c, fractional abundance; Branched glycerol monoalkyl glycerol tetraethers, H1048; Branched glycerol monoalkyl glycerol tetraethers, H1048, fractional abundance; brGMGTs; Conductivity, electrical; DATE/TIME; H-brGDGTs; Lake_Chala; Lake Chala; Lake Chala, East Africa; Month; MULT; Multiple investigations; Oxygen, dissolved; pH; Sample ID; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2629 data points
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    DATA PANGAEA
  • 68
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    Freshwater cultured pearls from Kentucky Lake - Table S2 (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: This Dataset serves as supplementary table S2 for our publication (Farfan et al, 2021). It contains all of the mineralogical, oxygen isotope, and Kentucky Lake environmental data compiled for the study, set into nacre-transect space defined by the SIMS-pits taken during oxygen isotope analyses.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Ammonia; Ammonia, standard deviation; aragonite; Chlorine; Chlorine, standard deviation; Conductivity, electrolytic; Conductivity, standard deviation; DATE/TIME; Depth, error; Depth with 1% of photosynthetic active radiation; Distance; Event label; Fractionation factor; Fractionation factor, error; Full width at half maximum; KentuckyLakePearl_1; KentuckyLakePearl_2; KentuckyLakePearl_3; LAKE; Light intensity; Light intensity, standard deviation; mineralogy; Nitrate and Nitrite; Nitrate and Nitrite, standard deviation; Oxidation reduction (RedOx) potential; Oxidation reduction (RedOx) potential, standard deviation; Oxygen, dissolved; Oxygen, dissolved, standard deviation; oxygen isotope; Peak centre; Peak height; pearls; pH; pH, standard deviation; Raman spectrometry; Raman spectroscopy; Ratio; Sample ID; Sampling lake; Secondary ion mass spectrometry (SIMS); Silicon dioxide; Silicon dioxide, standard deviation; Standard deviation; Sulfate; Sulfate, standard deviation; Temperature, standard deviation; Temperature, water; Thickness; Thickness, standard error; Transect; Turbidity, standard deviation; Turbidity (Nephelometric turbidity unit); δ18O; δ18O, aragonite; δ18O, standard error
    Type: Dataset
    Format: text/tab-separated-values, 29870 data points
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    DATA PANGAEA
  • 69
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    Hydrography measured from June 2009 - October 2020 in the Kiel Fjord, Germany (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: Five sites across the Kiel Fjord in the Baltic Sea (GEOMAR Pier: 54.330383 N 10.150683 E, Kiel Canal Entry: 54.361167 N, 10.162533 E, Falckenstein: 54.390217 N, 10.194983 E, Laboe: 54.405633 N, 10.209750 E, and Strande: 54.428267 N, 10.209267 E) were monitored biweekly from June 2013 until October 2020 (with some discontinuities in winter). Depth profiles were taken with a CTD (Sea & Sun Technology, Trappenkamp, CTD 60) recording temperature, salinity, pH, oxygen concentration as well as oxygen saturation. Oxygen and pH were corrected for temperature and salinity based on Standard Data Acquisition SSDA (C)opyright by SST 1999-2006. To avoid showing wrong measurements of the CTD probe, thresholds for the measured parameters were set (Temperature ≤ 25 °C, 8 ≤ Salinity ≥ 23, 5 ≤ pH ≥10, 0 mg L-1 ≤ Oxygen concentration ≥ 12 mg L-1 and 0% ≤ Oxygen Saturation ≥ 120%). Only those values were kept in the data set that did not exceed or fell below these thresholds. Furthermore, station specific depth limits were set (GEOMAR Pier ≤ 19 m, Kiel Canal Entry ≤ 13 m, Falckenstein ≤ 16 m, Laboe ≤ 17 m and Strande ≤ 17 m) and date exceeding of falling below these limits were excluded from the data set.
    Keywords: Baltic Sea; CTD/Rosette; CTD 60 (Sea & Sun Technology GmbH, Germany); CTD-RO; DATE/TIME; DEPTH, water; Event label; Latitude of event; Longitude of event; Oxygen; Oxygen saturation; pH; Salinity; Site_Falckenstein; Site_GEOMAR_Pier; Site_Kiel_Canal_Entry; Site_Laboe; Site_Strande; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1935236 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 70
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship HAFNIA SEA (July- December 2017) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Hafnia Sea (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Hafnia_North-Sea; Hafnia20170712; HAFNIA SEA; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 819286 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 71
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (February/March 2015) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20150221; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 196315 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 72
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (February 2018- January 2019) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20180202; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 1822524 data points
    Location Call Number Expected Availability
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  • 73
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship HAFNIA SEA (January-October 2016) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Hafnia Sea (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments / Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Hafnia_North-Sea; Hafnia20160120; HAFNIA SEA; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 678792 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 74
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (September 2013- January 2014) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20130914; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 599953 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 75
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (June- December 2015) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20150620; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 1096947 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 76
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    Particle fluxes at a sediment trap in the Vazella pourtalesii glass sponge grounds of the Scotian Shelf (2017-2018) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-10
    Description: The Scotian Shelf harbors unique aggregations of the glass sponge Vazella pourtalesii providing an important habitat for benthic and pelagic fauna. Recent studies have shown that these sponge grounds have persisted in the face of strong inter-annual and multi-decadal variability in temperature and salinity. However, little is known of the environmental characteristics on hourly-seasonal time scales. This study presents the first hydrodynamic observations and associated (food) particle supply mechanisms for the Vazella sponge grounds, highlighting the influence of natural variability in environmental conditions on sponge growth and resilience. Near-bottom environmental conditions were characterized by high temporal resolution data collected with a benthic lander, deployed during a period of 10-months in the Sambro Bank Sponge Conservation Area. The lander was equipped with temperature and oxygen sensors, a current meter, a sediment trap and a video camera. In addition, water column profiles of temperature and salinity were recorded along a transect, conducted in a gradient from high to lower sponge presence probability. Over the course of the lander deployment, temperature fluctuated between 8.8-12 °C with an average of 10.6 °C ± 0.4 °C. The water contained on average 6.3 mg l-1 oxygen and near bottom current speed was on average 0.12 m/s, with peaks up to 0.47 m/s. Semi-diurnal tidal flow was observed to result in constant resuspension of particulate matter in the benthic boundary layer. Surface storm events episodically caused extremely turbid conditions on the seafloor that persisted for several days, with particles being resuspended to more than 13 m above the seabed. The carbon flux in the near-bottom sediment trap peaked during storm events and also after a spring bloom in April, when fresh phytodetritus was observed in the bottom boundary layer. While resuspension events can represent a major stressor for sponges, limiting their filtration capability and remobilizing them, episodes of strong currents and lateral particle transport likely play an important role in food supply and the replenishment of nutrients and oxygen. Our results contextualize human-induced threats such as bottom fishing and climate change by providing more knowledge of the natural environmental conditions under which sponge grounds persist.
    Keywords: B_LANDER; Bottom lander; Carbon, flux; Carbon, organic, total; Carbon/Nitrogen ratio; DATE/TIME; Deep-sea Sponge Grounds Ecosystems of the North Atlantic; Delta V Advantage IRMS coupled to a Flash 2000 EA (EA-IRMS) by a 199 Conflo IV (Thermo Fisher Scientific Inc.); Martha L. Black; MLB2017001; MLB2017001_019; Nitrogen, total; SB_01; South Atlantic Ocean; SponGES; Technicap PPS4/3 181; Total mass, flux per day; δ13C; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 77
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship HAFNIA SEA (November 2016- June 2017) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Hafnia Sea (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments / Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Hafnia_North-Sea; Hafnia20160120; Hafnia20161128; HAFNIA SEA; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 847928 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 78
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (February- November 2014) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20140201; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 1789792 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 79
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    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (December 2015- December 2016) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20151210; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 1630512 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 80
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    Unknown
    FerryBox-integrated membrane-based pCO2, temperature and salinity sensor measurements from Cargo Ship LYSBRIS SEAWAYS (April 2017- January 2018) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-13
    Description: The submitted datasets contain surface seawater partial pressure of carbon dioxide (pCO2) values measured with Kongsberg Contros/4H-Jena HydroC-FT membrane-based sensors. These sensors were integrated on the FerryBox installed on the commercial vessel Lysbris Seaways (DFDS Seaways shipping company) travelling in the North Sea and maintained by the Coastal Research group at the Helmholtz-Zentrum Geesthacht, Germany. The pCO2 data were reprocessed from the raw data and corrected for sensor post-calibration where this was available. The instrument produces a result every second. 20-second averages are used for calculations and reported. Temperature and salinity results are also provided where available. These were measured from the underway with Falmouth Scientific Instruments/ Teledyne Instruments sensors also integrated with the FerryBox. The sensors were regularly maintained and occasionally replaced.
    Keywords: CONTROS HydroC CO2 FT sensor; DATE/TIME; FBOX; FerryBox; Helmholtz-Zentrum Geesthacht, Institute of Coastal Research; Hereon; HZG; LATITUDE; LONGITUDE; Lysbris_North-Sea; Lysbris20170407; LYSBRIS SEAWAYS; North Sea; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pCO2; Salinity; Salinity sensor (Teledyne RD Instruments); Temperature, water; Temperature sensor (Falmouth Scientific)
    Type: Dataset
    Format: text/tab-separated-values, 1201830 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 81
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    Unknown
    Wet chemistry analysis for soil organic carbon, pH, sand, silt, and clay content from samples in Lora del Rio, Andalusia, Spain (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: AUG; Auger; Carbon, organic; Clay; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Laboratory code/label; LATITUDE; LONGITUDE; Lora_del_Rio; Lora del Rio, Analusia, Spain; pH; ResourceCultures; Sand; SFB1070; Silt
    Type: Dataset
    Format: text/tab-separated-values, 760 data points
    Location Call Number Expected Availability
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  • 82
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    Unknown
    IPL isoGDGT concentration in SPM from Lake Chala, East Africa (Table S2) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Archaea; Conductivity, electrical; DATE/TIME; DEPTH, water; isoGDGTs; Isoprenoid acyclic glycerol dialkyl glycerol tetraether (peak area); Lake_Chala; Lake Chala; Lake Chala, East Africa; MULT; Multiple investigations; Oxygen, dissolved; pH; Sample ID; Settling particles; SPM; Temperature, water; Ultrahigh-performance liquid chromatography (UHPLC)
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
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  • 83
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    Unknown
    Predicted soil data from samples in Lora del Rio, Andalusia, Spain (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: AUG; Auger; Carbon, organic; Cation exchange capacity; Clay; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Laboratory code/label; LATITUDE; LONGITUDE; Lora_del_Rio; Lora del Rio, Analusia, Spain; pH; ResourceCultures; Sand; SFB1070; Silt; Water content, volumetric
    Type: Dataset
    Format: text/tab-separated-values, 5130 data points
    Location Call Number Expected Availability
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  • 84
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    Soil health indicators for Central Washington Orchards (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: The objective of this study was to initiate the steps to develop a soil assessment tool for irrigated orchard soils in Central Washington, United States including defining objectives, gathering baseline data and selecting target indicators. A total of 97 apple (Malus domestica) orchard fields were sampled in Washington, United States between 2015 and 2020. Of these plots there were 30 matched pairs (60 plots) on the same or similar soil type with matching cultivar/rootstock, tree age and training system type. One field in each pair was high performing and the other underperforming based on grower description. A subset of 32 plots (16 matched pairs) were sampled for fruit yield and fruit quality. Soil samples were collected as 50 to 100-soil core composite samples (2.5 cm core) to a depth of 20 cm in the tree root zone (15-60 cm from trunk) where 10 to 20 random samples were taken in each of five locations of the 2 to 16 hectare field. Four 100 cm3 intact soil cores were used for bulk density analysis. Five 120 cm3 intact cores were taken for micro-arthropod analysis. All soil sampling was conducted during June and July after soils had warmed (〉13 °C) and 1 to 3 months before apple harvest. Water supply for each orchard site was determined using a grower survey of irrigation practices and on-site irrigation measurements and demand was estimated from evapotranspiration estimates based on meteorological data from the nearest weather station [1]. On site irrigation measurements included measurements of water volume per emitter per hour at ten locations within a block which was then multiplied by emitters per acre. Fields with insufficient irrigation were not included in matched plot analysis. Fruit yield and quality were determined by collecting grower reported packing house yield data for the previous two to four years where available. For orchards where packing house data was not collected, a subset of five representative trees were selected for each orchard. At harvest, fruit per tree were counted and 20 fruit per tree collected to determine mean fruit weight and to estimate total yield. Yield was normalized to a 0-100 scale (percent yield goal) where the reported yield was divided by the yield goal identified by the grower in order to account for the yield potential of individual varieties and growing systems.
    Keywords: Apple bioassay; Apple bioassay rating; Apple rootstock; Apple scion; Autoclaved-citrate extractable soil protein index; Autoclaved-citrate extractable soil protein rating; Available water capacity; Available water capacity rating; Basal index; Basal Index rating; Bean bioassay rating; Bean bioassay scale; biological activity; Block; Calcium; Calcium rating; Calculated; Calculated according to DuPont et al. (2021); Carbon dioxide production; Cation exchange capacity; Cation exchange capacity rating; Central Washington, United States; Clay; CO2 release during a four day incubation of air dried and rewetted soil (Zibilske L 1994); Copper; Counted per 500 cm**3 of soil; Counted per m**2 (Crossley, DA 1991); Density, bulk rating; Density, dry bulk; DTPA-Sorbitol Extractable; Enrichment index; Enrichment index rating; Event label; Infiltration rate; Infiltration rating; Iron; Irrigation stress; Labile fraction of total P extraction with sodium bicarbonate after Olsen, 1954; LATITUDE; Lesion, Pratylenchus nematodes; Lesion, Xiphenema nematodes; LONGITUDE; Loss on ignition per Gavlack R (2005); Magnesium; Magnesium rating; Manganese; Measured by inserting five 15 cm diameter rings into the soil in the weed free strip beneath the trees to a depth of 7 cm; Microarthropods; Microarthropods rating; Micronutrients rating; Nematode soil food web analysis (Ferris and Bongers (1993)); Number; Organic matter rating; Penetration resistance; Penetration resistance rating; Percentage; Permanganate oxidation method (Weil 2003); Permanganate oxidizable carbon per soil dry mass; Permanganate oxidizable carbon rating; pH; Phosphorus; Phosphorus rating; pH rating; Plot; Potassium; Potassium rating; Potentially mineralizable nitrogen; Potentially mineralizable nitrogen rating; Pratylenchus nematodes rating; Pressure chambers and ceramic plates with a known porosity per Reynolds WD (2008); Rainfall simulator method per Kettler TA (2001); Rapid soil texture procedure per Kettler TA (2001); Rating; Respiration rating; Root disease symptoms rating per Abawi, Ludwig (2004); root health; Sample comment; Sand; Sand rating; Saturated, anaerobic incubation per Schindelbeck RR (2016); see comment; Seedling growth; Silt; Sodium bicarbonate K extraction; Sodium citrate protein extraction after Walker JM (2002); soil health; Soil name; soil organic carbon; Soil organic matter; soil quality; SOILS; Soil sample; soil structure; Soil texture; Soil texture classification; Structure index; Structure index rating; Tree, age; Tree density; USA NRCS soil survey; Washington_apple_orchard_AB242; Washington_apple_orchard_AB243; Washington_apple_orchard_AB40; Washington_apple_orchard_AB41; Washington_apple_orchard_Al88; Washington_apple_orchard_Al89; Washington_apple_orchard_AR64; Washington_apple_orchard_AR65; Washington_apple_orchard_B1; Washington_apple_orchard_B13; Washington_apple_orchard_B2; Washington_apple_orchard_Bk32; Washington_apple_orchard_Bk33; Washington_apple_orchard_Br27; Washington_apple_orchard_Br28; Washington_apple_orchard_Cl34; Washington_apple_orchard_Cl35; Washington_apple_orchard_CS74; Washington_apple_orchard_CS75; Washington_apple_orchard_Cw17; Washington_apple_orchard_Cw18; Washington_apple_orchard_DS72; Washington_apple_orchard_DS73; Washington_apple_orchard_F10; Washington_apple_orchard_F46; Washington_apple_orchard_F47; Washington_apple_orchard_F9; Washington_apple_orchard_G3; Washington_apple_orchard_G4; Washington_apple_orchard_Gil278; Washington_apple_orchard_Gil279; Washington_apple_orchard_Gil380; Washington_apple_orchard_Gil381; Washington_apple_orchard_Gil4100; Washington_apple_orchard_Gil4101; Washington_apple_orchard_Gil76; Washington_apple_orchard_Gil77; Washington_apple_orchard_GO60; Washington_apple_orchard_GO61; Washington_apple_orchard_H90; Washington_apple_orchard_H91; Washington_apple_orchard_Hou38; Washington_apple_orchard_Hou39; Washington_apple_orchard_K54; Washington_apple_orchard_K55; Washington_apple_orchard_KG48; Washington_apple_orchard_KG49; Washington_apple_orchard_KMO68; Washington_apple_orchard_KMO69; Washington_apple_orchard_M14; Washington_apple_orchard_M15; Washington_apple_orchard_MJ16; Washington_apple_orchard_O50; Washington_apple_orchard_O51; Washington_apple_orchard_Ob86; Washington_apple_orchard_Ob87; Washington_apple_orchard_P21; Washington_apple_orchard_P22; Washington_apple_orchard_R11; Washington_apple_orchard_R12; Washington_apple_orchard_Rb58; Washington_apple_orchard_Rb59; Washington_apple_orchard_S70; Washington_apple_orchard_S71; Washington_apple_orchard_SF36; Washington_apple_orchard_SF37; Washington_apple_orchard_SR29; Washington_apple_orchard_SR30; Washington_apple_orchard_SR31; Washington_apple_orchard_SRO92; Washington_apple_orchard_SRO93; Washington_apple_orchard_SRO94; Washington_apple_orchard_SRO95; Washington_apple_orchard_SRO96; Washington_apple_orchard_SRO97; Washington_apple_orchard_SRO98; Washington_apple_orchard_T62; Washington_apple_orchard_T63; Washington_apple_orchard_Th7; Washington_apple_orchard_Th8; Washington_apple_orchard_Va84; Washington_apple_orchard_Va85; Washington_apple_orchard_WA19; Washington_apple_orchard_WA20; Washington_apple_orchard_WAF56; Washington_apple_orchard_WAF57; Washington_apple_orchard_Wi44; Washington_apple_orchard_Wi45; Washington_apple_orchard_Zi266; Washington_apple_orchard_Zi267; Washington_apple_orchard_Zi382; Washington_apple_orchard_Zi383; Washington_apple_orchard_Zi4102; Washington_apple_orchard_Zi4103; Washington_apple_orchard_Zi52; Washington_apple_orchard_Zi53; Water stable aggregates; Water stable aggregates rating; Xiphenema nematodes rating; Year of observation; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 7203 data points
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  • 85
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    Water chemistry of unfiltered groundwater samples from the Fennoscandian Shield deep terrestrial biosphere in 2018 and 2019 (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: Copious amounts of organic carbon are stored for long periods of time in deep continental groundwaters. Little is known about its composition and cycling, mainly due to the difficulties in obtaining sample material. Cool fracture waters of different origins can be obtained under clean conditions at Äspö Hard Rock Laboratory (Äspö HRL, Sweden), operated by the Swedish Nuclear Fuel and Waste Management Company (SKB). We sampled groundwater from different depth (171 to 507 meter below sea level) in the bedrock fractures in November 2018 and March-April 2019. We assessed water chemistry and dissolved organic matter composition via stable carbon isotopic and molecular-formula level analysis in recent Baltic Sea-influenced to old saline fracture waters in the granitic Fennoscandian shield. Physicochemical parameters, major ions, water isotopic compositions (δ18O and δD), total nitrogen as well as dissolved organic matter concentration and stable isotopic composition were obtained for unfiltered groundwater samples from different boreholes.
    Keywords: aquifer; BalticSea_Äspö; BalticSea_Kalmar; Calcium; Carbon, organic, dissolved; Carbon, organic, dissolved, standard deviation; Carbon-14, modern, dissolved inorganic carbon; Carbon-14, modern, dissolved organic carbon; Chlorine; Conductivity; DATE/TIME; Elevation of event; Event label; Extraction efficiency; FT-ICR-MS; groundwater; HA2780A_1; Iron; Iron, total; Iron 2+; KA1755A_3; KA2051A01_5; KA2511A_5; KA2862A_1; KA2865A01_1; KA3105A_3; KA3385A_1; KA3510A_2; KA3600F_2; Latitude of event; Longitude of event; Magnesium; Manganese; Nitrogen, total dissolved; Nitrogen, total dissolved, standard deviation; Nitrogen in ammonium; Nitrogen in nitrate; Nitrogen in nitrite; pH; Phosphorus in phosphate; Potassium; SA1229A_1; SA1730A_1; SA2600A_1; Sodium; Sulfide in hydrogen sulfide; Sulfur in sulfate; Sweden; Temperature, water; Type; δ13C, dissolved inorganic carbon; δ13C, dissolved organic carbon; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 1050 data points
    Location Call Number Expected Availability
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  • 86
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    Unknown
    Chemical and isotope data for porewater samples from Paleochori Bay, Milos, Greece (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Description: Despite more than 25 years of research, the spatial and temporal variability of hydrothermal venting in Paleochori Bay remains poorly constrained because there are no reliable repeat measurements at discrete locations. Using a georeferenced photographic map of Paleochori Bay (https://doi.org/10.1594/PANGAEA.915881), scuba divers collected 168 porewater and seawater samples inside and outside of the bay and exact GPS coordinates were recorded for each sample. The GPS coordinates of the sampling locations should provide a foundation for future research in Paleochori Bay by enabling reliable repeat measurements. The dataset was combined with the temperature measurements previously reported (https://doi.org/10.1594/PANGAEA.915881) and contains chemical, isotopic data, as well as water depth and sediment color. All porewater samples were taken at a sediment depth of 0.1 m.
    Keywords: Arsenic; Bromine; Calcium; Chlorine; Color description; DEPTH, water; DIVER; Event label; Iron; Latitude of event; Lithium; Longitude of event; M001; M002; M003; M004; M005; M006; M007; M008; M009; M010; M011; M012; M013; M014; M015; M016; M017; M018; M019; M020; M021; M022; M023; M024; M025; M026; M028; M029; M030; M031; M032; M033; M034; M035; M036; M037; M038; M039; M040; M041; M042; M043; M044; M045; M046; M047; M048; M049; M050; M051; M052; M053; M054; M055; M056; M057; M058; M059; M060; M061; M062; M063; M064; M065; M066; M067; M068; M069; M070; M071; M072; M073; M074; M075; M076; M077; M078; M079; M080; M081; M082; M083; M084; M085; M086; M087; M088; M089; M090; M091; M092; M093; M094; M095; M096; M097; M098; M099; M100; M101; M102; M103; M104; M105; M107; M108; M109; M110; M111; M112; M113; M114; M115; M117; M118; M119; M120; M121; M122; M123; M124; M125; M126; M127; M128; M129; M130; M131; M132; M133; M134; M135; M136; M137; M138; M139; M140; M141; M142; M143; M144; M145; M146; M147; M148; M149; M150; M151; M152; M153; M154; M155; M156; M157; M158; M159; M160; M161; M162; M163; M164; M165; M166; M167; M168; Magnesium; Manganese; Palaeochori Bay, Milos, Greece; pH; Potassium; Sample type; Sampling by diver; Silicon; Sodium; Strontium; Sulfate; Temperature, water; δ18O, water; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 3126 data points
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    DATA PANGAEA
  • 87
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    Unknown
    Position and vehicle attitude of ROV at station ALERT2018_22_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Position and vehicle attitude of ROV obtained on First-Year-Ice (FYI) and Multi-Year-Ice (MYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 22 May 2018.
    Keywords: ALERT2018; ALERT2018_22_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land
    Type: Dataset
    Format: text/tab-separated-values, 117720 data points
    Location Call Number Expected Availability
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  • 88
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    Incident spectral solar irradiance measured above sea ice at ROV station ALERT2018_10_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Measurements of solar radiation over sea ice have been performed on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 10 May 2018. The radiation measurements have been performed with Ramses spectral radiometers (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) was installed on the sea ice for surface reference measurements (solar irradiance). All times are given in UTC.
    Keywords: ALERT2018; ALERT2018_10_1; ALTITUDE; Calculated; DATE/TIME; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; Irradiance, incident; Irradiance, incident, photosynthetically active; Irradiance, incident, photosynthetically active, absolute; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Spectral irradiance, incident at 320 nm; Spectral irradiance, incident at 321 nm; Spectral irradiance, incident at 322 nm; Spectral irradiance, incident at 323 nm; Spectral irradiance, incident at 324 nm; Spectral irradiance, incident at 325 nm; Spectral irradiance, incident at 326 nm; Spectral irradiance, incident at 327 nm; Spectral irradiance, incident at 328 nm; Spectral irradiance, incident at 329 nm; Spectral irradiance, incident at 330 nm; Spectral irradiance, incident at 331 nm; Spectral irradiance, incident at 332 nm; Spectral irradiance, incident at 333 nm; Spectral irradiance, incident at 334 nm; Spectral irradiance, incident at 335 nm; Spectral irradiance, incident at 336 nm; Spectral irradiance, incident at 337 nm; Spectral irradiance, incident at 338 nm; Spectral irradiance, incident at 339 nm; Spectral irradiance, incident at 340 nm; Spectral irradiance, incident at 341 nm; Spectral irradiance, incident at 342 nm; Spectral irradiance, incident at 343 nm; Spectral irradiance, incident at 344 nm; Spectral irradiance, incident at 345 nm; Spectral irradiance, incident at 346 nm; Spectral irradiance, incident at 347 nm; Spectral irradiance, incident at 348 nm; Spectral irradiance, incident at 349 nm; Spectral irradiance, incident at 350 nm; Spectral irradiance, incident at 351 nm; Spectral irradiance, incident at 352 nm; Spectral irradiance, incident at 353 nm; Spectral irradiance, incident at 354 nm; Spectral irradiance, incident at 355 nm; Spectral irradiance, incident at 356 nm; Spectral irradiance, incident at 357 nm; Spectral irradiance, incident at 358 nm; Spectral irradiance, incident at 359 nm; Spectral irradiance, incident at 360 nm; Spectral irradiance, incident at 361 nm; Spectral irradiance, incident at 362 nm; Spectral irradiance, incident at 363 nm; Spectral irradiance, incident at 364 nm; Spectral irradiance, incident at 365 nm; Spectral irradiance, incident at 366 nm; Spectral irradiance, incident at 367 nm; Spectral irradiance, incident at 368 nm; Spectral irradiance, incident at 369 nm; Spectral irradiance, incident at 370 nm; Spectral irradiance, incident at 371 nm; Spectral irradiance, incident at 372 nm; Spectral irradiance, incident at 373 nm; Spectral irradiance, incident at 374 nm; Spectral irradiance, incident at 375 nm; Spectral irradiance, incident at 376 nm; Spectral irradiance, incident at 377 nm; Spectral irradiance, incident at 378 nm; Spectral irradiance, incident at 379 nm; Spectral irradiance, incident at 380 nm; Spectral irradiance, incident at 381 nm; Spectral irradiance, incident at 382 nm; Spectral irradiance, incident at 383 nm; Spectral irradiance, incident at 384 nm; Spectral irradiance, incident at 385 nm; Spectral irradiance, incident at 386 nm; Spectral irradiance, incident at 387 nm; Spectral irradiance, incident at 388 nm; Spectral irradiance, incident at 389 nm; Spectral irradiance, incident at 390 nm; Spectral irradiance, incident at 391 nm; Spectral irradiance, incident at 392 nm; Spectral irradiance, incident at 393 nm; Spectral irradiance, incident at 394 nm; Spectral irradiance, incident at 395 nm; Spectral irradiance, incident at 396 nm; Spectral irradiance, incident at 397 nm; Spectral irradiance, incident at 398 nm; Spectral irradiance, incident at 399 nm; Spectral irradiance, incident at 400 nm; Spectral irradiance, incident at 401 nm; Spectral irradiance, incident at 402 nm; Spectral irradiance, incident at 403 nm; Spectral irradiance, incident at 404 nm; Spectral irradiance, incident at 405 nm; Spectral irradiance, incident at 406 nm; Spectral irradiance, incident at 407 nm; Spectral irradiance, incident at 408 nm; Spectral irradiance, incident at 409 nm; Spectral irradiance, incident at 410 nm; Spectral irradiance, incident at 411 nm; Spectral irradiance, incident at 412 nm; Spectral irradiance, incident at 413 nm; Spectral irradiance, incident at 414 nm; Spectral irradiance, incident at 415 nm; Spectral irradiance, incident at 416 nm; Spectral irradiance, incident at 417 nm; Spectral irradiance, incident at 418 nm; Spectral irradiance, incident at 419 nm; Spectral irradiance, incident at 420 nm; Spectral irradiance, incident at 421 nm; Spectral irradiance, incident at 422 nm; Spectral irradiance, incident at 423 nm; Spectral irradiance, incident at 424 nm; Spectral irradiance, incident at 425 nm; Spectral irradiance, incident at 426 nm; Spectral irradiance, incident at 427 nm; Spectral irradiance, incident at 428 nm; Spectral irradiance, incident at 429 nm; Spectral irradiance, incident at 430 nm; Spectral irradiance, incident at 431 nm; Spectral irradiance, incident at 432 nm; Spectral irradiance, incident at 433 nm; Spectral irradiance, incident at 434 nm; Spectral irradiance, incident at 435 nm; Spectral irradiance, incident at 436 nm; Spectral irradiance, incident at 437 nm; Spectral irradiance, incident at 438 nm; Spectral irradiance, incident at 439 nm; Spectral irradiance, incident at 440 nm; Spectral irradiance, incident at 441 nm; Spectral irradiance, incident at 442 nm; Spectral irradiance, incident at 443 nm; Spectral irradiance, incident at 444 nm; Spectral irradiance, incident at 445 nm; Spectral irradiance, incident at 446 nm; Spectral irradiance, incident at 447 nm; Spectral irradiance, incident at 448 nm; Spectral irradiance, incident at 449 nm; Spectral irradiance, incident at 450 nm; Spectral irradiance, incident at 451 nm; Spectral irradiance, incident at 452 nm; Spectral irradiance, incident at 453 nm; Spectral irradiance, incident at 454 nm; Spectral irradiance, incident at 455 nm; Spectral irradiance, incident at 456 nm; Spectral irradiance, incident at 457 nm; Spectral irradiance, incident at 458 nm; Spectral irradiance, incident at 459 nm; Spectral irradiance, incident at 460 nm; Spectral irradiance, incident at 461 nm; Spectral irradiance, incident at 462 nm; Spectral irradiance, incident at 463 nm; Spectral irradiance, incident at 464 nm; Spectral irradiance, incident at 465 nm; Spectral irradiance, incident at 466 nm; Spectral irradiance, incident at 467 nm; Spectral irradiance, incident at 468 nm; Spectral irradiance, incident at 469 nm; Spectral irradiance, incident at 470 nm; Spectral irradiance, incident at 471 nm; Spectral irradiance, incident at 472 nm; Spectral irradiance, incident at 473 nm; Spectral irradiance, incident at 474 nm; Spectral irradiance, incident at 475 nm; Spectral irradiance, incident at 476 nm; Spectral irradiance, incident at 477 nm; Spectral irradiance, incident at 478 nm; Spectral irradiance, incident at 479 nm; Spectral irradiance, incident at 480 nm; Spectral irradiance, incident at 481 nm; Spectral irradiance, incident at 482 nm; Spectral irradiance, incident at 483 nm; Spectral irradiance, incident at 484 nm; Spectral irradiance, incident at 485 nm; Spectral irradiance, incident at 486 nm; Spectral irradiance, incident at 487 nm; Spectral irradiance, incident at 488 nm; Spectral irradiance, incident at 489 nm; Spectral irradiance, incident at 490 nm; Spectral irradiance, incident at 491 nm; Spectral irradiance, incident at 492 nm; Spectral irradiance, incident at 493 nm; Spectral irradiance, incident at 494 nm; Spectral irradiance, incident at 495 nm; Spectral irradiance, incident at 496 nm; Spectral irradiance, incident at 497 nm; Spectral irradiance, incident at 498 nm; Spectral irradiance, incident at 499 nm; Spectral irradiance, incident at 500 nm; Spectral irradiance, incident at 501 nm; Spectral irradiance, incident at 502 nm; Spectral irradiance, incident at 503 nm; Spectral irradiance, incident at 504 nm; Spectral irradiance, incident at 505 nm; Spectral irradiance, incident at
    Type: Dataset
    Format: text/tab-separated-values, 1701022 data points
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    DATA PANGAEA
  • 89
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    Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at ROV station ALERT2018_22_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Measurements of transmitted irradiance under sea ice have been performed on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 22 May 2018. The radiation measurements have been performed with Ramses spectral radiometers (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) for energy budget calculations was installed on the ROV. All times are given in UTC.
    Keywords: ALERT2018; ALERT2018_22_1; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; Irradiance, downward; Irradiance, downward, photosynthetically active; Irradiance, downward, photosynthetically active, absolute; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Spectral irradiance, downward at 320 nm; Spectral irradiance, downward at 321 nm; Spectral irradiance, downward at 322 nm; Spectral irradiance, downward at 323 nm; Spectral irradiance, downward at 324 nm; Spectral irradiance, downward at 325 nm; Spectral irradiance, downward at 326 nm; Spectral irradiance, downward at 327 nm; Spectral irradiance, downward at 328 nm; Spectral irradiance, downward at 329 nm; Spectral irradiance, downward at 330 nm; Spectral irradiance, downward at 331 nm; Spectral irradiance, downward at 332 nm; Spectral irradiance, downward at 333 nm; Spectral irradiance, downward at 334 nm; Spectral irradiance, downward at 335 nm; Spectral irradiance, downward at 336 nm; Spectral irradiance, downward at 337 nm; Spectral irradiance, downward at 338 nm; Spectral irradiance, downward at 339 nm; Spectral irradiance, downward at 340 nm; Spectral irradiance, downward at 341 nm; Spectral irradiance, downward at 342 nm; Spectral irradiance, downward at 343 nm; Spectral irradiance, downward at 344 nm; Spectral irradiance, downward at 345 nm; Spectral irradiance, downward at 346 nm; Spectral irradiance, downward at 347 nm; Spectral irradiance, downward at 348 nm; Spectral irradiance, downward at 349 nm; Spectral irradiance, downward at 350 nm; Spectral irradiance, downward at 351 nm; Spectral irradiance, downward at 352 nm; Spectral irradiance, downward at 353 nm; Spectral irradiance, downward at 354 nm; Spectral irradiance, downward at 355 nm; Spectral irradiance, downward at 356 nm; Spectral irradiance, downward at 357 nm; Spectral irradiance, downward at 358 nm; Spectral irradiance, downward at 359 nm; Spectral irradiance, downward at 360 nm; Spectral irradiance, downward at 361 nm; Spectral irradiance, downward at 362 nm; Spectral irradiance, downward at 363 nm; Spectral irradiance, downward at 364 nm; Spectral irradiance, downward at 365 nm; Spectral irradiance, downward at 366 nm; Spectral irradiance, downward at 367 nm; Spectral irradiance, downward at 368 nm; Spectral irradiance, downward at 369 nm; Spectral irradiance, downward at 370 nm; Spectral irradiance, downward at 371 nm; Spectral irradiance, downward at 372 nm; Spectral irradiance, downward at 373 nm; Spectral irradiance, downward at 374 nm; Spectral irradiance, downward at 375 nm; Spectral irradiance, downward at 376 nm; Spectral irradiance, downward at 377 nm; Spectral irradiance, downward at 378 nm; Spectral irradiance, downward at 379 nm; Spectral irradiance, downward at 380 nm; Spectral irradiance, downward at 381 nm; Spectral irradiance, downward at 382 nm; Spectral irradiance, downward at 383 nm; Spectral irradiance, downward at 384 nm; Spectral irradiance, downward at 385 nm; Spectral irradiance, downward at 386 nm; Spectral irradiance, downward at 387 nm; Spectral irradiance, downward at 388 nm; Spectral irradiance, downward at 389 nm; Spectral irradiance, downward at 390 nm; Spectral irradiance, downward at 391 nm; Spectral irradiance, downward at 392 nm; Spectral irradiance, downward at 393 nm; Spectral irradiance, downward at 394 nm; Spectral irradiance, downward at 395 nm; Spectral irradiance, downward at 396 nm; Spectral irradiance, downward at 397 nm; Spectral irradiance, downward at 398 nm; Spectral irradiance, downward at 399 nm; Spectral irradiance, downward at 400 nm; Spectral irradiance, downward at 401 nm; Spectral irradiance, downward at 402 nm; Spectral irradiance, downward at 403 nm; Spectral irradiance, downward at 404 nm; Spectral irradiance, downward at 405 nm; Spectral irradiance, downward at 406 nm; Spectral irradiance, downward at 407 nm; Spectral irradiance, downward at 408 nm; Spectral irradiance, downward at 409 nm; Spectral irradiance, downward at 410 nm; Spectral irradiance, downward at 411 nm; Spectral irradiance, downward at 412 nm; Spectral irradiance, downward at 413 nm; Spectral irradiance, downward at 414 nm; Spectral irradiance, downward at 415 nm; Spectral irradiance, downward at 416 nm; Spectral irradiance, downward at 417 nm; Spectral irradiance, downward at 418 nm; Spectral irradiance, downward at 419 nm; Spectral irradiance, downward at 420 nm; Spectral irradiance, downward at 421 nm; Spectral irradiance, downward at 422 nm; Spectral irradiance, downward at 423 nm; Spectral irradiance, downward at 424 nm; Spectral irradiance, downward at 425 nm; Spectral irradiance, downward at 426 nm; Spectral irradiance, downward at 427 nm; Spectral irradiance, downward at 428 nm; Spectral irradiance, downward at 429 nm; Spectral irradiance, downward at 430 nm; Spectral irradiance, downward at 431 nm; Spectral irradiance, downward at 432 nm; Spectral irradiance, downward at 433 nm; Spectral irradiance, downward at 434 nm; Spectral irradiance, downward at 435 nm; Spectral irradiance, downward at 436 nm; Spectral irradiance, downward at 437 nm; Spectral irradiance, downward at 438 nm; Spectral irradiance, downward at 439 nm; Spectral irradiance, downward at 440 nm; Spectral irradiance, downward at 441 nm; Spectral irradiance, downward at 442 nm; Spectral irradiance, downward at 443 nm; Spectral irradiance, downward at 444 nm; Spectral irradiance, downward at 445 nm; Spectral irradiance, downward at 446 nm; Spectral irradiance, downward at 447 nm; Spectral irradiance, downward at 448 nm; Spectral irradiance, downward at 449 nm; Spectral irradiance, downward at 450 nm; Spectral irradiance, downward at 451 nm; Spectral irradiance, downward at 452 nm; Spectral irradiance, downward at 453 nm; Spectral irradiance, downward at 454 nm; Spectral irradiance, downward at 455 nm; Spectral irradiance, downward at 456 nm; Spectral irradiance, downward at 457 nm; Spectral irradiance, downward at 458 nm; Spectral irradiance, downward at 459 nm; Spectral irradiance, downward at 460 nm; Spectral irradiance, downward at 461 nm; Spectral irradiance, downward at 462 nm; Spectral irradiance, downward at 463 nm; Spectral irradiance, downward at 464 nm; Spectral irradiance, downward at 465 nm; Spectral irradiance, downward at 466 nm; Spectral irradiance, downward at 467 nm; Spectral irradiance, downward at 468 nm; Spectral irradiance, downward at 469 nm; Spectral irradiance, downward at 470 nm; Spectral irradiance, downward at 471 nm; Spectral irradiance, downward at 472 nm; Spectral irradiance, downward at 473 nm; Spectral irradiance, downward at 474 nm; Spectral irradiance, downward at 475 nm; Spectral irradiance, downward at 476 nm; Spectral irradiance, downward at 477 nm; Spectral irradiance, downward at 478 nm; Spectral irradiance, downward at 479 nm; Spectral irradiance, downward at 480 nm; Spectral irradiance, downward at 481 nm; Spectral irradiance, downward at 482 nm; Spectral irradiance, downward at 483 nm; Spectral irradiance, downward at 484 nm; Spectral irradiance, downward at 485 nm; Spectral irradiance, downward at 486 nm; Spectral irradiance, downward at 487 nm; Spectral irradiance, downward at 488 nm; Spectral irradiance, downward at 489 nm; Spectral irradiance, downward at 490 nm; Spectral irradiance, downward at 491 nm; Spectral irradiance, downward at 492 nm; Spectral irradiance, downward at 493 nm; Spectral irradiance, downward at 494 nm; Spectral irradiance, downward at 495 nm; Spectral irradiance, downward at 496 nm; Spectral irradiance, downward at 497 nm; Spectral irradiance, downward at 498 nm; Spectral irradiance, downward at 499 nm; Spectral irradiance, downward at 500 nm; Spectral irradiance, downward at 501 nm; Spectral irradiance, downward at 502 nm; Spectral irradiance, downward at 503 nm; Spectral irradiance, downward at 504 nm; Spectral irradiance,
    Type: Dataset
    Format: text/tab-separated-values, 1149897 data points
    Location Call Number Expected Availability
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  • 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 ALERT2018_10_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Measurements of transmitted radiance under sea ice and corresponding incident solar radiation at the surface have been performed on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 10 May 2018. The radiation measurements have been performed with Ramses spectral radiometers (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The radiance sensor (9° opening angle) was installed on the ROV. The transflectance is the ratio between transmitted radiance and incident irradiance. All times are given in UTC.
    Keywords: ALERT2018; ALERT2018_10_1; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; 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;
    Type: Dataset
    Format: text/tab-separated-values, 1667101 data points
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  • 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 ALERT2018_22_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Measurements of transmitted radiance under sea ice and corresponding incident solar radiation at the surface have been performed on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 22 May 2018. The radiation measurements have been performed with Ramses spectral radiometers (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The radiance sensor (9° opening angle) was installed on the ROV. The transflectance is the ratio between transmitted radiance and incident irradiance. All times are given in UTC.
    Keywords: ALERT2018; ALERT2018_22_1; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; 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;
    Type: Dataset
    Format: text/tab-separated-values, 1492356 data points
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  • 92
    facet.materialart.
    Unknown
    Times when the ROV passed along the underice markers M0 to M10 as obtained from a high definition zoom video camera at ROV station ALERT2018_22_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Times when the ROV passed along the underice markers M0 to M10 as obtained from a high definition zoom video camera (Surveyor HD, Teledyne Bowtech, Aberdeen, UK) as obtained on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 12 and 22 May 2018. Manual post-processing of the position was required because it was distorted probably because sound speed differences were not taken into account during surveys. To correct this distortion, we used the times when the ROV passed along the underice markers M0 to M10 which positions were known from GPS measurements at the surface. The ROV was kept in a stable position at the markers between start and end time. The markers were each separated by 10 m and distributed along a 100 m transect.
    Keywords: ALERT2018; ALERT2018_22_1; Date/time end; Date/time start; Distance, relative, X; Distance, relative, Y; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 93
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    Unknown
    GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica (GPS_low) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; Antarctica; ANT-Land_2016/17_FISP; ANT-Land_2016/17_FISP_GPS_low; AWI Antarctic Land Expedition; DATE/TIME; Filchner Ice Shelf; Filchner Ice Shelf Project; FISP; GNSS; GPS; GPSR; GPS receiver; LATITUDE; LONGITUDE; Melt Channel; Waypoint GravNav 8.8 processing software
    Type: Dataset
    Format: text/tab-separated-values, 0 data points
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  • 94
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    Unknown
    GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica (GPS_ow) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; Antarctica; ANT-Land_2016/17_FISP; ANT-Land_2016/17_FISP_GPS_ow; AWI Antarctic Land Expedition; DATE/TIME; Filchner Ice Shelf; Filchner Ice Shelf Project; FISP; GNSS; GPS; GPSR; GPS receiver; LATITUDE; LONGITUDE; Melt Channel; Waypoint GravNav 8.8 processing software
    Type: Dataset
    Format: text/tab-separated-values, 0 data points
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  • 95
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    Unknown
    GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica (GPS_oe) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; Antarctica; ANT-Land_2016/17_FISP; ANT-Land_2016/17_FISP_GPS_oe; AWI Antarctic Land Expedition; DATE/TIME; Filchner Ice Shelf; Filchner Ice Shelf Project; FISP; GNSS; GPS; GPSR; GPS receiver; LATITUDE; LONGITUDE; Melt Channel; Waypoint GravNav 8.8 processing software
    Type: Dataset
    Format: text/tab-separated-values, 0 data points
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  • 96
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    Unknown
    GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica (GPS_se_long) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; Antarctica; ANT-Land_2015/16_FISP; ANT-Land_2015/16_FISP_GPS_se_long; AWI Antarctic Land Expedition; DATE/TIME; Filchner Ice Shelf; Filchner Ice Shelf Project; FISP; GNSS; GPS; GPSR; GPS receiver; LATITUDE; LONGITUDE; Melt Channel; Waypoint GravNav 8.8 processing software
    Type: Dataset
    Format: text/tab-separated-values, 0 data points
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  • 97
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    Unknown
    GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica (GPS_se) (2021)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; Antarctica; ANT-Land_2016/17_FISP; ANT-Land_2016/17_FISP_GPS_se; AWI Antarctic Land Expedition; DATE/TIME; Filchner Ice Shelf; Filchner Ice Shelf Project; FISP; GNSS; GPS; GPSR; GPS receiver; LATITUDE; LONGITUDE; Melt Channel; Waypoint GravNav 8.8 processing software
    Type: Dataset
    Format: text/tab-separated-values, 0 data points
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  • 98
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    Unknown
    Marine electrical resistivity profile 4 - east, Bykovsky Peninsula, Siberia (2021)
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    Details
    Publication Date: 2023-03-16
    Description: The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset between the first electrode and the boat was approximately 10 m.
    Keywords: Alas; AWI Arctic Land Expedition; BYK_profile4e_parallel_to_shore; Bykovsky; DEPTH, water; electrical resistivity; Electrical resistivity tomography; ERT; LATITUDE; Lena2017; Lena Delta; LONGITUDE; Near surface geophysics; PETA-CARB; POINT DISTANCE from start; Position; Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool; Resistivity, apparent; Resistivity profiler, IRIS Syscal Pro Deep Marine; RU-Land_2017_Lena; Submarine Permafrost; subsea permafrost; talik; Thermokarst Lagoon
    Type: Dataset
    Format: text/tab-separated-values, 920 data points
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  • 99
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    Unknown
    Position and vehicle attitude of ROV at station ALERT2018_12_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Position and vehicle attitude of ROV obtained on First-Year-Ice (FYI) and Multi-Year-Ice (MYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 12 May 2018.
    Keywords: ALERT2018; ALERT2018_12_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land
    Type: Dataset
    Format: text/tab-separated-values, 104330 data points
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  • 100
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    Unknown
    Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at ROV station ALERT2018_10_1 (2021)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: Measurements of transmitted irradiance under sea ice have been performed on First-Year-Ice (FYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea on 10 May 2018. The radiation measurements have been performed with Ramses spectral radiometers (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) for energy budget calculations was installed on the ROV. All times are given in UTC.
    Keywords: ALERT2018; ALERT2018_10_1; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; Irradiance, downward; Irradiance, downward, photosynthetically active; Irradiance, downward, photosynthetically active, absolute; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Spectral irradiance, downward at 320 nm; Spectral irradiance, downward at 321 nm; Spectral irradiance, downward at 322 nm; Spectral irradiance, downward at 323 nm; Spectral irradiance, downward at 324 nm; Spectral irradiance, downward at 325 nm; Spectral irradiance, downward at 326 nm; Spectral irradiance, downward at 327 nm; Spectral irradiance, downward at 328 nm; Spectral irradiance, downward at 329 nm; Spectral irradiance, downward at 330 nm; Spectral irradiance, downward at 331 nm; Spectral irradiance, downward at 332 nm; Spectral irradiance, downward at 333 nm; Spectral irradiance, downward at 334 nm; Spectral irradiance, downward at 335 nm; Spectral irradiance, downward at 336 nm; Spectral irradiance, downward at 337 nm; Spectral irradiance, downward at 338 nm; Spectral irradiance, downward at 339 nm; Spectral irradiance, downward at 340 nm; Spectral irradiance, downward at 341 nm; Spectral irradiance, downward at 342 nm; Spectral irradiance, downward at 343 nm; Spectral irradiance, downward at 344 nm; Spectral irradiance, downward at 345 nm; Spectral irradiance, downward at 346 nm; Spectral irradiance, downward at 347 nm; Spectral irradiance, downward at 348 nm; Spectral irradiance, downward at 349 nm; Spectral irradiance, downward at 350 nm; Spectral irradiance, downward at 351 nm; Spectral irradiance, downward at 352 nm; Spectral irradiance, downward at 353 nm; Spectral irradiance, downward at 354 nm; Spectral irradiance, downward at 355 nm; Spectral irradiance, downward at 356 nm; Spectral irradiance, downward at 357 nm; Spectral irradiance, downward at 358 nm; Spectral irradiance, downward at 359 nm; Spectral irradiance, downward at 360 nm; Spectral irradiance, downward at 361 nm; Spectral irradiance, downward at 362 nm; Spectral irradiance, downward at 363 nm; Spectral irradiance, downward at 364 nm; Spectral irradiance, downward at 365 nm; Spectral irradiance, downward at 366 nm; Spectral irradiance, downward at 367 nm; Spectral irradiance, downward at 368 nm; Spectral irradiance, downward at 369 nm; Spectral irradiance, downward at 370 nm; Spectral irradiance, downward at 371 nm; Spectral irradiance, downward at 372 nm; Spectral irradiance, downward at 373 nm; Spectral irradiance, downward at 374 nm; Spectral irradiance, downward at 375 nm; Spectral irradiance, downward at 376 nm; Spectral irradiance, downward at 377 nm; Spectral irradiance, downward at 378 nm; Spectral irradiance, downward at 379 nm; Spectral irradiance, downward at 380 nm; Spectral irradiance, downward at 381 nm; Spectral irradiance, downward at 382 nm; Spectral irradiance, downward at 383 nm; Spectral irradiance, downward at 384 nm; Spectral irradiance, downward at 385 nm; Spectral irradiance, downward at 386 nm; Spectral irradiance, downward at 387 nm; Spectral irradiance, downward at 388 nm; Spectral irradiance, downward at 389 nm; Spectral irradiance, downward at 390 nm; Spectral irradiance, downward at 391 nm; Spectral irradiance, downward at 392 nm; Spectral irradiance, downward at 393 nm; Spectral irradiance, downward at 394 nm; Spectral irradiance, downward at 395 nm; Spectral irradiance, downward at 396 nm; Spectral irradiance, downward at 397 nm; Spectral irradiance, downward at 398 nm; Spectral irradiance, downward at 399 nm; Spectral irradiance, downward at 400 nm; Spectral irradiance, downward at 401 nm; Spectral irradiance, downward at 402 nm; Spectral irradiance, downward at 403 nm; Spectral irradiance, downward at 404 nm; Spectral irradiance, downward at 405 nm; Spectral irradiance, downward at 406 nm; Spectral irradiance, downward at 407 nm; Spectral irradiance, downward at 408 nm; Spectral irradiance, downward at 409 nm; Spectral irradiance, downward at 410 nm; Spectral irradiance, downward at 411 nm; Spectral irradiance, downward at 412 nm; Spectral irradiance, downward at 413 nm; Spectral irradiance, downward at 414 nm; Spectral irradiance, downward at 415 nm; Spectral irradiance, downward at 416 nm; Spectral irradiance, downward at 417 nm; Spectral irradiance, downward at 418 nm; Spectral irradiance, downward at 419 nm; Spectral irradiance, downward at 420 nm; Spectral irradiance, downward at 421 nm; Spectral irradiance, downward at 422 nm; Spectral irradiance, downward at 423 nm; Spectral irradiance, downward at 424 nm; Spectral irradiance, downward at 425 nm; Spectral irradiance, downward at 426 nm; Spectral irradiance, downward at 427 nm; Spectral irradiance, downward at 428 nm; Spectral irradiance, downward at 429 nm; Spectral irradiance, downward at 430 nm; Spectral irradiance, downward at 431 nm; Spectral irradiance, downward at 432 nm; Spectral irradiance, downward at 433 nm; Spectral irradiance, downward at 434 nm; Spectral irradiance, downward at 435 nm; Spectral irradiance, downward at 436 nm; Spectral irradiance, downward at 437 nm; Spectral irradiance, downward at 438 nm; Spectral irradiance, downward at 439 nm; Spectral irradiance, downward at 440 nm; Spectral irradiance, downward at 441 nm; Spectral irradiance, downward at 442 nm; Spectral irradiance, downward at 443 nm; Spectral irradiance, downward at 444 nm; Spectral irradiance, downward at 445 nm; Spectral irradiance, downward at 446 nm; Spectral irradiance, downward at 447 nm; Spectral irradiance, downward at 448 nm; Spectral irradiance, downward at 449 nm; Spectral irradiance, downward at 450 nm; Spectral irradiance, downward at 451 nm; Spectral irradiance, downward at 452 nm; Spectral irradiance, downward at 453 nm; Spectral irradiance, downward at 454 nm; Spectral irradiance, downward at 455 nm; Spectral irradiance, downward at 456 nm; Spectral irradiance, downward at 457 nm; Spectral irradiance, downward at 458 nm; Spectral irradiance, downward at 459 nm; Spectral irradiance, downward at 460 nm; Spectral irradiance, downward at 461 nm; Spectral irradiance, downward at 462 nm; Spectral irradiance, downward at 463 nm; Spectral irradiance, downward at 464 nm; Spectral irradiance, downward at 465 nm; Spectral irradiance, downward at 466 nm; Spectral irradiance, downward at 467 nm; Spectral irradiance, downward at 468 nm; Spectral irradiance, downward at 469 nm; Spectral irradiance, downward at 470 nm; Spectral irradiance, downward at 471 nm; Spectral irradiance, downward at 472 nm; Spectral irradiance, downward at 473 nm; Spectral irradiance, downward at 474 nm; Spectral irradiance, downward at 475 nm; Spectral irradiance, downward at 476 nm; Spectral irradiance, downward at 477 nm; Spectral irradiance, downward at 478 nm; Spectral irradiance, downward at 479 nm; Spectral irradiance, downward at 480 nm; Spectral irradiance, downward at 481 nm; Spectral irradiance, downward at 482 nm; Spectral irradiance, downward at 483 nm; Spectral irradiance, downward at 484 nm; Spectral irradiance, downward at 485 nm; Spectral irradiance, downward at 486 nm; Spectral irradiance, downward at 487 nm; Spectral irradiance, downward at 488 nm; Spectral irradiance, downward at 489 nm; Spectral irradiance, downward at 490 nm; Spectral irradiance, downward at 491 nm; Spectral irradiance, downward at 492 nm; Spectral irradiance, downward at 493 nm; Spectral irradiance, downward at 494 nm; Spectral irradiance, downward at 495 nm; Spectral irradiance, downward at 496 nm; Spectral irradiance, downward at 497 nm; Spectral irradiance, downward at 498 nm; Spectral irradiance, downward at 499 nm; Spectral irradiance, downward at 500 nm; Spectral irradiance, downward at 501 nm; Spectral irradiance, downward at 502 nm; Spectral irradiance, downward at 503 nm; Spectral irradiance, downward at 504 nm; Spectral irradiance,
    Type: Dataset
    Format: text/tab-separated-values, 1296813 data points
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