Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data
Abstract Geothermal heat flow is a key parameter in governing ice dynamics, via its influence on basal melt and sliding, englacial rheology, and erosion. It is expected to exhibit significant lateral variability across Antarctica. Despite this, surface heat flow derived from Earth's interior re...
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Online Access: | https://doi.org/10.1029/2023GL106274 https://doaj.org/article/53a5f2820e954e63b76f801a7b3c3a6b |
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ftdoajarticles:oai:doaj.org/article:53a5f2820e954e63b76f801a7b3c3a6b 2024-09-15T17:48:17+00:00 Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data James A. N. Hazzard Fred D. Richards 2024-04-01T00:00:00Z https://doi.org/10.1029/2023GL106274 https://doaj.org/article/53a5f2820e954e63b76f801a7b3c3a6b EN eng Wiley https://doi.org/10.1029/2023GL106274 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106274 https://doaj.org/article/53a5f2820e954e63b76f801a7b3c3a6b Geophysical Research Letters, Vol 51, Iss 7, Pp n/a-n/a (2024) geothermal heat flow seismological data mantle structure inverse methods uncertainty anelasticity Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2023GL106274 2024-08-05T17:49:23Z Abstract Geothermal heat flow is a key parameter in governing ice dynamics, via its influence on basal melt and sliding, englacial rheology, and erosion. It is expected to exhibit significant lateral variability across Antarctica. Despite this, surface heat flow derived from Earth's interior remains one of the most poorly constrained parameters controlling ice sheet evolution. To obtain a continent‐wide map of Antarctic heat supply at regional‐scale resolution, we estimate upper mantle thermomechanical structure directly from VS. Until now, direct inferences of Antarctic heat supply have assumed constant crustal composition. Here, we explore a range of crustal conductivity and radiogenic heat production values by fitting thermodynamically self‐consistent geotherms to their seismically inferred counterparts. Independent estimates of crustal conductivity derived from VP are integrated to break an observed trade‐off between crustal parameters, allowing us to infer Antarctic geothermal heat flow and its associated uncertainty. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 51 7 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
geothermal heat flow seismological data mantle structure inverse methods uncertainty anelasticity Geophysics. Cosmic physics QC801-809 |
spellingShingle |
geothermal heat flow seismological data mantle structure inverse methods uncertainty anelasticity Geophysics. Cosmic physics QC801-809 James A. N. Hazzard Fred D. Richards Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
topic_facet |
geothermal heat flow seismological data mantle structure inverse methods uncertainty anelasticity Geophysics. Cosmic physics QC801-809 |
description |
Abstract Geothermal heat flow is a key parameter in governing ice dynamics, via its influence on basal melt and sliding, englacial rheology, and erosion. It is expected to exhibit significant lateral variability across Antarctica. Despite this, surface heat flow derived from Earth's interior remains one of the most poorly constrained parameters controlling ice sheet evolution. To obtain a continent‐wide map of Antarctic heat supply at regional‐scale resolution, we estimate upper mantle thermomechanical structure directly from VS. Until now, direct inferences of Antarctic heat supply have assumed constant crustal composition. Here, we explore a range of crustal conductivity and radiogenic heat production values by fitting thermodynamically self‐consistent geotherms to their seismically inferred counterparts. Independent estimates of crustal conductivity derived from VP are integrated to break an observed trade‐off between crustal parameters, allowing us to infer Antarctic geothermal heat flow and its associated uncertainty. |
format |
Article in Journal/Newspaper |
author |
James A. N. Hazzard Fred D. Richards |
author_facet |
James A. N. Hazzard Fred D. Richards |
author_sort |
James A. N. Hazzard |
title |
Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
title_short |
Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
title_full |
Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
title_fullStr |
Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
title_full_unstemmed |
Antarctic Geothermal Heat Flow, Crustal Conductivity and Heat Production Inferred From Seismological Data |
title_sort |
antarctic geothermal heat flow, crustal conductivity and heat production inferred from seismological data |
publisher |
Wiley |
publishDate |
2024 |
url |
https://doi.org/10.1029/2023GL106274 https://doaj.org/article/53a5f2820e954e63b76f801a7b3c3a6b |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_source |
Geophysical Research Letters, Vol 51, Iss 7, Pp n/a-n/a (2024) |
op_relation |
https://doi.org/10.1029/2023GL106274 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106274 https://doaj.org/article/53a5f2820e954e63b76f801a7b3c3a6b |
op_doi |
https://doi.org/10.1029/2023GL106274 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
7 |
_version_ |
1810289446794297344 |