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  • Greenland  (1)
  • Ice extent; IceExtSiegert1999; LATITUDE; LONGITUDE; modelled; Quaternary Environment of the Eurasian North; QUEEN; QUEENModels; RECON; Reconstructed data  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Siegert, Martin J; Dowdeswell, Julian A; Melles, Martin (1999): Late Weichselian glaciation of the Russian High Arctic. Quaternary Research, 52(3), 273-285, https://doi.org/10.1006/qres.1999.2082
    Publication Date: 2023-05-12
    Description: A numerical ice-sheet model was used to reconstruct the Late Weichselian glaciation of the Eurasian High Arctic, between Franz Josef Land and Severnaya Zemlya. An ice sheet was developed over the entire Eurasian High Arctic so that ice flow from the central Barents and Kara seas toward the northern Russian Arctic could be accounted for. An inverse approach to modeling was utilized, where ice-sheet results were forced to be compatible with geological information indicating ice-free conditions over the Taymyr Peninsula during the Late Weichselian. The model indicates complete glaciation of the Barents and Kara seas and predicts a “maximum-sized” ice sheet for the Late Weichselian Russian High Arctic. In this scenario, full-glacial conditions are characterized by a 1500-m-thick ice mass over the Barents Sea, from which ice flowed to the north and west within several bathymetric troughs as large ice streams. In contrast to this reconstruction, a “minimum” model of glaciation involves restricted glaciation in the Kara Sea, where the ice thickness is only 300 m in the south and which is free of ice in the north across Severnaya Zemlya. Our maximum reconstruction is compatible with geological information that indicates complete glaciation of the Barents Sea. However, geological data from Severnaya Zemlya suggest our minimum model is more relevant further east. This, in turn, implies a strong paleoclimatic gradient to colder and drier conditions eastward across the Eurasian Arctic during the Late Weichselian.
    Keywords: Ice extent; IceExtSiegert1999; LATITUDE; LONGITUDE; modelled; Quaternary Environment of the Eurasian North; QUEEN; QUEENModels; RECON; Reconstructed data
    Type: Dataset
    Format: text/tab-separated-values, 4859 data points
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  • 2
    Publication Date: 2022-05-26
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geophysical Research Letters 44 (2017): 11,051–11,061, doi:10.1002/2017GL074954.
    Description: Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the penetration of warm Atlantic water (AW) that rapidly melts and undercuts Greenland's marine-terminating glaciers. Here we present a new compilation of Greenland bed topography that assimilates seafloor bathymetry and ice thickness data through a mass conservation approach. A new 150 m horizontal resolution bed topography/bathymetric map of Greenland is constructed with seamless transitions at the ice/ocean interface, yielding major improvements over previous data sets, particularly in the marine-terminating sectors of northwest and southeast Greenland. Our map reveals that the total sea level potential of the Greenland ice sheet is 7.42 ± 0.05 m, which is 7 cm greater than previous estimates. Furthermore, it explains recent calving front response of numerous outlet glaciers and reveals new pathways by which AW can access glaciers with marine-based basins, thereby highlighting sectors of Greenland that are most vulnerable to future oceanic forcing.
    Description: National Aeronautics and Space Administration; Cryospheric Sciences Program Grant Number: NNX15AD55G; National Science Foundation's ARCSS program Grant Number: 1504230; NERC Grant Number: NE/M000869/1
    Keywords: Greenland ; Bathymetry ; Mass conservation ; Multibeam echo sounding ; Radar echo sounding ; Glaciology
    Repository Name: Woods Hole Open Access Server
    Type: Article
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