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...

Full description

Bibliographic Details
Main Authors: Chris J. Carson, Sandra McLaren, Jason L. Roberts, Steven D. Boger, Donald D. Blankenship
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