Greenland and Canadian Arctic ice temperature profiles database
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Published:2023-09-08
Issue:9
Volume:17
Page:3829-3845
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Løkkegaard AnjaORCID, Mankoff Kenneth D.ORCID, Zdanowicz ChristianORCID, Clow Gary D.ORCID, Lüthi Martin P.ORCID, Doyle Samuel H.ORCID, Thomsen Henrik H., Fisher David, Harper JoelORCID, Aschwanden AndyORCID, Vinther Bo M., Dahl-Jensen Dorthe, Zekollari HarryORCID, Meierbachtol Toby, McDowell IanORCID, Humphrey Neil, Solgaard AnneORCID, Karlsson Nanna B.ORCID, Khan Shfaqat A.ORCID, Hills BenjaminORCID, Law RobertORCID, Hubbard BrynORCID, Christoffersen PoulORCID, Jacquemart MylèneORCID, Seguinot JulienORCID, Fausto Robert S.ORCID, Colgan William T.ORCID
Abstract
Abstract. Here, we present a compilation of 95 ice temperature profiles from 85 boreholes from the Greenland ice sheet and peripheral ice caps, as well as local ice caps in the Canadian Arctic. Profiles from only 31 boreholes (36 %) were previously available in open-access data repositories. The remaining 54 borehole profiles (64 %) are being made digitally available here for the first time. These newly available profiles, which are associated with pre-2010 boreholes, have been submitted by community members or digitized from published graphics and/or data tables. All 95 profiles are now made available in both absolute (meters) and normalized (0 to 1 ice thickness) depth scales and are accompanied by extensive metadata. These metadata include a transparent description of data provenance. The ice temperature profiles span 70 years, with the earliest profile being from 1950 at Camp VI, West Greenland. To highlight the value of this database in evaluating ice flow simulations, we compare the ice temperature profiles from the Greenland ice sheet with an ice flow simulation by the Parallel Ice Sheet Model (PISM). We find a cold bias in modeled near-surface ice temperatures within the ablation area, a warm bias in modeled basal ice temperatures at inland cold-bedded sites, and an apparent underestimation of deformational heating in high-strain settings. These biases provide process level insight on simulated ice temperatures.
Funder
Danmarks Frie Forskningsfond Villum Fonden Fonds De La Recherche Scientifique - FNRS Horizon 2020 Natural Environment Research Council Goddard Institute for Space Studies Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung Office of Polar Programs
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
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