Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica
Numerical models are the primary predictive tools for understanding the dynamic behaviour of the Antarctic ice sheet. However, a key boundary parameter, sub-glacial heat flow, remains poorly constrained. We show that variations in abundance and distribution of heat-producing elements within the Anta...
Main Authors: | , , , , |
---|---|
Format: | Other Non-Article Part of Journal/Newspaper |
Language: | unknown |
Published: |
2016
|
Subjects: | |
Online Access: | https://doi.org/10.6084/m9.figshare.3453554.v1 https://figshare.com/articles/Hot_rocks_in_a_cold_place_high_sub-glacial_heat_flow_in_East_Antarctica/3453554 |
id |
ftgeosoclonfig:oai:figshare.com:article/3453554 |
---|---|
record_format |
openpolar |
spelling |
ftgeosoclonfig:oai:figshare.com:article/3453554 2023-05-15T13:33:01+02:00 Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica Chris J. Carson Sandra McLaren Jason L. Roberts Steven D. Boger Donald D. Blankenship 2016-06-21T11:30:32Z https://doi.org/10.6084/m9.figshare.3453554.v1 https://figshare.com/articles/Hot_rocks_in_a_cold_place_high_sub-glacial_heat_flow_in_East_Antarctica/3453554 unknown doi:10.6084/m9.figshare.3453554.v1 https://figshare.com/articles/Hot_rocks_in_a_cold_place_high_sub-glacial_heat_flow_in_East_Antarctica/3453554 CC BY 4.0 CC-BY Geology Antarctic ice sheet heat flow crust result heat flows ice modelling studies ice mass balance boundary parameter East Antarctica Numerical models Hot rocks ice sheet behaviour Text Journal contribution 2016 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.3453554.v1 2020-02-21T07:24:10Z Numerical models are the primary predictive tools for understanding the dynamic behaviour of the Antarctic ice sheet. However, a key boundary parameter, sub-glacial heat flow, remains poorly constrained. We show that variations in abundance and distribution of heat-producing elements within the Antarctic continental crust result in greater and more variable regional sub-glacial heat flows than currently assumed in ice modelling studies. Such elevated heat flows would have a fundamental effect on ice sheet behaviour and highlight that geological controls on heat flow must be considered to obtain more accurate and refined predictions of ice mass balance and sea-level change. Other Non-Article Part of Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Geological Society of London: Figshare Antarctic East Antarctica The Antarctic |
institution |
Open Polar |
collection |
Geological Society of London: Figshare |
op_collection_id |
ftgeosoclonfig |
language |
unknown |
topic |
Geology Antarctic ice sheet heat flow crust result heat flows ice modelling studies ice mass balance boundary parameter East Antarctica Numerical models Hot rocks ice sheet behaviour |
spellingShingle |
Geology Antarctic ice sheet heat flow crust result heat flows ice modelling studies ice mass balance boundary parameter East Antarctica Numerical models Hot rocks ice sheet behaviour Chris J. Carson Sandra McLaren Jason L. Roberts Steven D. Boger Donald D. Blankenship Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
topic_facet |
Geology Antarctic ice sheet heat flow crust result heat flows ice modelling studies ice mass balance boundary parameter East Antarctica Numerical models Hot rocks ice sheet behaviour |
description |
Numerical models are the primary predictive tools for understanding the dynamic behaviour of the Antarctic ice sheet. However, a key boundary parameter, sub-glacial heat flow, remains poorly constrained. We show that variations in abundance and distribution of heat-producing elements within the Antarctic continental crust result in greater and more variable regional sub-glacial heat flows than currently assumed in ice modelling studies. Such elevated heat flows would have a fundamental effect on ice sheet behaviour and highlight that geological controls on heat flow must be considered to obtain more accurate and refined predictions of ice mass balance and sea-level change. |
format |
Other Non-Article Part of Journal/Newspaper |
author |
Chris J. Carson Sandra McLaren Jason L. Roberts Steven D. Boger Donald D. Blankenship |
author_facet |
Chris J. Carson Sandra McLaren Jason L. Roberts Steven D. Boger Donald D. Blankenship |
author_sort |
Chris J. Carson |
title |
Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
title_short |
Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
title_full |
Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
title_fullStr |
Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
title_full_unstemmed |
Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica |
title_sort |
hot rocks in a cold place: high sub-glacial heat flow in east antarctica |
publishDate |
2016 |
url |
https://doi.org/10.6084/m9.figshare.3453554.v1 https://figshare.com/articles/Hot_rocks_in_a_cold_place_high_sub-glacial_heat_flow_in_East_Antarctica/3453554 |
geographic |
Antarctic East Antarctica The Antarctic |
geographic_facet |
Antarctic East Antarctica The Antarctic |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
op_relation |
doi:10.6084/m9.figshare.3453554.v1 https://figshare.com/articles/Hot_rocks_in_a_cold_place_high_sub-glacial_heat_flow_in_East_Antarctica/3453554 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.3453554.v1 |
_version_ |
1766037751677845504 |