Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean

The thermal state of the lithosphere and related geothermal heat flow (GHF) is a crucial parameter to understand a variety of processes related to cryospheric, geospheric, and/or biospheric interactions. Indirect estimates of GHF in polar regions from magnetic, seismological, or petrological data of...

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Published in:Geosciences
Main Authors: Ricarda Dziadek, Mechthild Doll, Fynn Warnke, Vera Schlindwein
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/geosciences11010011
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spelling ftmdpi:oai:mdpi.com:/2076-3263/11/1/11/ 2023-08-20T04:02:10+02:00 Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean Ricarda Dziadek Mechthild Doll Fynn Warnke Vera Schlindwein agris 2020-12-27 application/pdf https://doi.org/10.3390/geosciences11010011 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/geosciences11010011 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 11; Issue 1; Pages: 11 geothermal heat flow in situ temperature measurements Antarctica Arctic Ocean Weddell Sea Powell Basin Gakkel Ridge Aurora Vent Field Text 2020 ftmdpi https://doi.org/10.3390/geosciences11010011 2023-08-01T00:44:34Z The thermal state of the lithosphere and related geothermal heat flow (GHF) is a crucial parameter to understand a variety of processes related to cryospheric, geospheric, and/or biospheric interactions. Indirect estimates of GHF in polar regions from magnetic, seismological, or petrological data often show large discrepancies when compared to thermal in situ observations. Here, the lack of in situ data represents a fundamental limitation for both investigating thermal processes of the lithosphere and validating indirect heat flow estimates. During RV Polarstern expeditions PS86 and PS118, we obtained in situ thermal measurements and present the derived GHF in key regions, such as the Antarctic Peninsula and the Gakkel Ridge in the Arctic. By comparison with indirect models, our results indicate (1) elevated geothermal heat flow (75 ± 5 mW m−2 to 139 ± 26 mW m−2) to the west of the Antarctic Peninsula, which should be considered for future investigations of ice-sheet dynamics and the visco-elastic behavior of the crust. (2) The thermal signature of the Powell Basin characteristic for oceanic crust of an age between 32 and 18 Ma. Further, we propose (3) that at different heat sources at the slow-spreading Gakkel Ridge in the Aurora Vent Field region might explain the geothermal heat flow distribution. We conclude that in situ observations are urgently required to ground-truth and fine-tune existing models and that a multidisciplinary approach is of high importance for the scientific community’s understanding of this parameter. Text Antarc* Antarctic Antarctic Peninsula Antarctica Arctic Arctic Ocean Ice Sheet Weddell Sea MDPI Open Access Publishing Antarctic Antarctic Peninsula Arctic Arctic Ocean Gakkel Ridge ENVELOPE(90.000,90.000,87.000,87.000) Powell Basin ENVELOPE(-49.500,-49.500,-62.250,-62.250) The Antarctic Weddell Weddell Sea Geosciences 11 1 11
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic geothermal heat flow
in situ temperature measurements
Antarctica
Arctic Ocean
Weddell Sea
Powell Basin
Gakkel Ridge
Aurora Vent Field
spellingShingle geothermal heat flow
in situ temperature measurements
Antarctica
Arctic Ocean
Weddell Sea
Powell Basin
Gakkel Ridge
Aurora Vent Field
Ricarda Dziadek
Mechthild Doll
Fynn Warnke
Vera Schlindwein
Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
topic_facet geothermal heat flow
in situ temperature measurements
Antarctica
Arctic Ocean
Weddell Sea
Powell Basin
Gakkel Ridge
Aurora Vent Field
description The thermal state of the lithosphere and related geothermal heat flow (GHF) is a crucial parameter to understand a variety of processes related to cryospheric, geospheric, and/or biospheric interactions. Indirect estimates of GHF in polar regions from magnetic, seismological, or petrological data often show large discrepancies when compared to thermal in situ observations. Here, the lack of in situ data represents a fundamental limitation for both investigating thermal processes of the lithosphere and validating indirect heat flow estimates. During RV Polarstern expeditions PS86 and PS118, we obtained in situ thermal measurements and present the derived GHF in key regions, such as the Antarctic Peninsula and the Gakkel Ridge in the Arctic. By comparison with indirect models, our results indicate (1) elevated geothermal heat flow (75 ± 5 mW m−2 to 139 ± 26 mW m−2) to the west of the Antarctic Peninsula, which should be considered for future investigations of ice-sheet dynamics and the visco-elastic behavior of the crust. (2) The thermal signature of the Powell Basin characteristic for oceanic crust of an age between 32 and 18 Ma. Further, we propose (3) that at different heat sources at the slow-spreading Gakkel Ridge in the Aurora Vent Field region might explain the geothermal heat flow distribution. We conclude that in situ observations are urgently required to ground-truth and fine-tune existing models and that a multidisciplinary approach is of high importance for the scientific community’s understanding of this parameter.
format Text
author Ricarda Dziadek
Mechthild Doll
Fynn Warnke
Vera Schlindwein
author_facet Ricarda Dziadek
Mechthild Doll
Fynn Warnke
Vera Schlindwein
author_sort Ricarda Dziadek
title Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
title_short Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
title_full Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
title_fullStr Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
title_full_unstemmed Towards Closing the Polar Gap: New Marine Heat Flow Observations in Antarctica and the Arctic Ocean
title_sort towards closing the polar gap: new marine heat flow observations in antarctica and the arctic ocean
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/geosciences11010011
op_coverage agris
long_lat ENVELOPE(90.000,90.000,87.000,87.000)
ENVELOPE(-49.500,-49.500,-62.250,-62.250)
geographic Antarctic
Antarctic Peninsula
Arctic
Arctic Ocean
Gakkel Ridge
Powell Basin
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Antarctic Peninsula
Arctic
Arctic Ocean
Gakkel Ridge
Powell Basin
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Arctic
Arctic Ocean
Ice Sheet
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Arctic
Arctic Ocean
Ice Sheet
Weddell Sea
op_source Geosciences; Volume 11; Issue 1; Pages: 11
op_relation https://dx.doi.org/10.3390/geosciences11010011
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences11010011
container_title Geosciences
container_volume 11
container_issue 1
container_start_page 11
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