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Persistent Identifier
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doi:10.22008/FK2/RJNF92 |
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Publication Date
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2026-04-08 |
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Title
| Supplementary Files for: Community heat flow recommendations: suitable basal boundary conditions for Greenland and Antarctica in ISMIP7 |
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Author
| Lösing, Mareen (The University of Western Australia) - ORCID: https://orcid.org/0000-0002-9222-2107
Colgan, William (GEUS) - ORCID: https://orcid.org/0000-0001-6334-1660
Stål, Tobias (School of Natural Sciences (Physics), University of Tasmania, Hobart, Australia) - ORCID: https://orcid.org/0000-0002-4323-6748
Ebbing, Jörg (Institute of Geosciences, Kiel University, Germany) - ORCID: https://orcid.org/0000-0001-7492-5338
Busck, Anne G. (Department of Geosciences and Natural Resource Management, (IGN), Copenhagen University, Denmark) - ORCID: https://orcid.org/0000-0002-7328-795X
Zhang, Tong (State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction, Faculty of Geographical Science, Beijing Normal University, Beijing, China) - ORCID: https://orcid.org/0000-0001-9074-4166
Seroussi, Hélène L. (Thayer School of Engineering, Dartmouth College, Hanover, NH 03755, USA) - ORCID: https://orcid.org/0000-0001-9201-1644
McCormack, Felicity (Securing Antarctica's Environmental Future, School of Earth, Atmosphere & Environment, Monash University, Clayton, Kulin Nations, Victoria, Australia) - ORCID: https://orcid.org/0000-0002-2324-2120
Fahrner, Dominik (Department of Glaciology and Climate, Geological Survey of Denmark and Greenland, 1350, Copenhagen, Denmark) - ORCID: https://orcid.org/0000-0002-7895-1557
Stearns, Leigh (University of Pennsylvania, Philadelphia, USA) - ORCID: https://orcid.org/0000-0001-7358-7015
Svendsen, Synne H. (GEUS, Denmark) - ORCID: Svendsen
Reading, Anya (School of Natural Sciences (Physics), University of Tasmania, Hobart, Australia) - ORCID: https://orcid.org/0000-0002-9316-7605 |
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Point of Contact
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Use email button above to contact.
Witcombe, Nicola Anne (Geus.dk) |
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Description
| Geothermal heat flow (GHF) influences ice sheet thermal conditions, affecting ice flow by sliding and deformation. However, GHF distribution under polar ice sheets remains poorly constrained, with few direct borehole-derived estimates and large discrepancies between glaciological and geophysicalmodels caused by methodological differences and data limitations. As a result, many ice sheet models rely on uniform GHF estimates, ensemble averages or outdated fields that oversimplify reality. The choice of GHF product can lead to significantly different thermal conditions simulated at the ice-bed interface, which affects the projected evolution of ice sheets under climate warming. Therefore, we conducted an expert elicitation survey to identify the most suitable GHF fields for use as basal boundary conditions in ice sheet modelling, particularly for the Ice Sheet Modelling Intercomparison Project for CMIP7 (ISMIP7). GHF fields generally fall into three categories: (1) outdated due to improved data availability, (2) overly simplified parameterisations and (3) current and preferred. For GHF fields that rank highly in the survey, we discuss uncertainty, data dependency and provide guidance on their use in different applications. Finally, we recommend two Antarctic and one Greenlandic GHF field(s) for ISMIP7. |
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Subject
| Earth and Environmental Sciences |
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Keyword
| geothermal heat flow, basal boundary conditions, Ice sheet modelling (ISMIP7), Antarctica and Greenland, expert elicitation survey |
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Related Publication
| doi: 10.34194/r0w9rf81 |
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Depositor
| Witcombe, Nicola Anne |
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Deposit Date
| 2026-03-10 |