Antarctic geothermal heat flow and its implications for tectonics and ice sheets

Published online 26 October 2022 Geothermal heat flow (GHF) is an elusive physical property, yet it can reveal past and present plate tectonic processes. In Antarctica, GHF has further consequences in predicting the response of ice sheets to climate change. In this Review, we discuss variations in A...

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Published in:Nature Reviews Earth & Environment
Main Authors: Reading, A.M., Stål, T., Halpin, J.A., Lösing, M., Ebbing, J., Shen, W., McCormack, F.S., Siddoway, C.S., Hasterok, D.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Nature 2022
Subjects:
Online Access:https://hdl.handle.net/2440/136921
https://doi.org/10.1038/s43017-022-00348-y
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/136921 2023-12-17T10:21:37+01:00 Antarctic geothermal heat flow and its implications for tectonics and ice sheets Reading, A.M. Stål, T. Halpin, J.A. Lösing, M. Ebbing, J. Shen, W. McCormack, F.S. Siddoway, C.S. Hasterok, D. 2022 https://hdl.handle.net/2440/136921 https://doi.org/10.1038/s43017-022-00348-y en eng Springer Nature http://purl.org/au-research/grants/arc/DP190100418 http://purl.org/au-research/grants/arc/DP180104074 http://purl.org/au-research/grants/arc/DE210101433 NATURE REVIEWS EARTH & ENVIRONMENT, 2022; 3(12):814-831 2662-138X https://hdl.handle.net/2440/136921 doi:10.1038/s43017-022-00348-y Hasterok, D. [0000-0002-8257-7975] © 2022, Springer Nature Limited http://dx.doi.org/10.1038/s43017-022-00348-y Cryospheric science Geophysics Tectonics Journal article 2022 ftunivadelaidedl https://doi.org/10.1038/s43017-022-00348-y 2023-11-20T23:27:17Z Published online 26 October 2022 Geothermal heat flow (GHF) is an elusive physical property, yet it can reveal past and present plate tectonic processes. In Antarctica, GHF has further consequences in predicting the response of ice sheets to climate change. In this Review, we discuss variations in Antarctic GHF models based on geophysical methods and draw insights into tectonics and GHF model usage for ice sheet modelling. The inferred GHF at continental scale for West Antarctica (up to 119 mW m−2, 95th percentile) points to numerous contributing influences, including non-steady state neotectonic processes. Combined influences cause especially high values in the vicinity of the Thwaites Glacier, a location critical for the accurate prediction of accelerated loss of Antarctic ice mass. The inferred variations across East Antarctica are more subtle (up to 66 mW m−2, 95th percentile), where slightly elevated values in some locations correspond to the influence of thinned lithosphere and tectonic units with concentrations of heat-producing elements. Fine-scale anomalies owing to heat-producing elements and horizontal components of heat flow are important for regional modelling. GHF maps comprising central values with these fine-scale anomalies captured within uncertainty bounds can thus enable improved ensemble-based ice sheet model predictions of Antarctic ice loss. Anya M. Reading, Tobias Stål, Jacqueline A. Halpin, Mareen Lösing, Jörg Ebbing, Weisen Shen, Felicity S. McCormack, Christine S. Siddoway, Derrick Hasterok Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Thwaites Glacier West Antarctica The University of Adelaide: Digital Library Antarctic East Antarctica Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) West Antarctica Nature Reviews Earth & Environment 3 12 814 831
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
topic Cryospheric science
Geophysics
Tectonics
spellingShingle Cryospheric science
Geophysics
Tectonics
Reading, A.M.
Stål, T.
Halpin, J.A.
Lösing, M.
Ebbing, J.
Shen, W.
McCormack, F.S.
Siddoway, C.S.
Hasterok, D.
Antarctic geothermal heat flow and its implications for tectonics and ice sheets
topic_facet Cryospheric science
Geophysics
Tectonics
description Published online 26 October 2022 Geothermal heat flow (GHF) is an elusive physical property, yet it can reveal past and present plate tectonic processes. In Antarctica, GHF has further consequences in predicting the response of ice sheets to climate change. In this Review, we discuss variations in Antarctic GHF models based on geophysical methods and draw insights into tectonics and GHF model usage for ice sheet modelling. The inferred GHF at continental scale for West Antarctica (up to 119 mW m−2, 95th percentile) points to numerous contributing influences, including non-steady state neotectonic processes. Combined influences cause especially high values in the vicinity of the Thwaites Glacier, a location critical for the accurate prediction of accelerated loss of Antarctic ice mass. The inferred variations across East Antarctica are more subtle (up to 66 mW m−2, 95th percentile), where slightly elevated values in some locations correspond to the influence of thinned lithosphere and tectonic units with concentrations of heat-producing elements. Fine-scale anomalies owing to heat-producing elements and horizontal components of heat flow are important for regional modelling. GHF maps comprising central values with these fine-scale anomalies captured within uncertainty bounds can thus enable improved ensemble-based ice sheet model predictions of Antarctic ice loss. Anya M. Reading, Tobias Stål, Jacqueline A. Halpin, Mareen Lösing, Jörg Ebbing, Weisen Shen, Felicity S. McCormack, Christine S. Siddoway, Derrick Hasterok
format Article in Journal/Newspaper
author Reading, A.M.
Stål, T.
Halpin, J.A.
Lösing, M.
Ebbing, J.
Shen, W.
McCormack, F.S.
Siddoway, C.S.
Hasterok, D.
author_facet Reading, A.M.
Stål, T.
Halpin, J.A.
Lösing, M.
Ebbing, J.
Shen, W.
McCormack, F.S.
Siddoway, C.S.
Hasterok, D.
author_sort Reading, A.M.
title Antarctic geothermal heat flow and its implications for tectonics and ice sheets
title_short Antarctic geothermal heat flow and its implications for tectonics and ice sheets
title_full Antarctic geothermal heat flow and its implications for tectonics and ice sheets
title_fullStr Antarctic geothermal heat flow and its implications for tectonics and ice sheets
title_full_unstemmed Antarctic geothermal heat flow and its implications for tectonics and ice sheets
title_sort antarctic geothermal heat flow and its implications for tectonics and ice sheets
publisher Springer Nature
publishDate 2022
url https://hdl.handle.net/2440/136921
https://doi.org/10.1038/s43017-022-00348-y
long_lat ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Antarctic
East Antarctica
Thwaites Glacier
West Antarctica
geographic_facet Antarctic
East Antarctica
Thwaites Glacier
West Antarctica
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Thwaites Glacier
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Thwaites Glacier
West Antarctica
op_source http://dx.doi.org/10.1038/s43017-022-00348-y
op_relation http://purl.org/au-research/grants/arc/DP190100418
http://purl.org/au-research/grants/arc/DP180104074
http://purl.org/au-research/grants/arc/DE210101433
NATURE REVIEWS EARTH & ENVIRONMENT, 2022; 3(12):814-831
2662-138X
https://hdl.handle.net/2440/136921
doi:10.1038/s43017-022-00348-y
Hasterok, D. [0000-0002-8257-7975]
op_rights © 2022, Springer Nature Limited
op_doi https://doi.org/10.1038/s43017-022-00348-y
container_title Nature Reviews Earth & Environment
container_volume 3
container_issue 12
container_start_page 814
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