Antarctic Geothermal Heat Flow Model: Aq1

We present a refined map of geothermal heat flow for Antarctica, Aq1, based on multiple observables. The map is generated using a similarity detection approach by attributing observables from geophysics and geology to a large number of high‐quality heat flow values ( N =5,792) from other continents....

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Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Staal, T, Reading, AM, Halpin, JA, Whittaker, J
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2020
Subjects:
Online Access:https://doi.org/10.1029/2020GC009428
http://ecite.utas.edu.au/143094
id ftunivtasecite:oai:ecite.utas.edu.au:143094
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:143094 2023-05-15T13:42:40+02:00 Antarctic Geothermal Heat Flow Model: Aq1 Staal, T Reading, AM Halpin, JA Whittaker, J 2020 https://doi.org/10.1029/2020GC009428 http://ecite.utas.edu.au/143094 en eng Amer Geophysical Union http://dx.doi.org/10.1029/2020GC009428 Staal, T and Reading, AM and Halpin, JA and Whittaker, J, Antarctic Geothermal Heat Flow Model: Aq1, Geochemistry, Geophysics, Geosystems, 22, (2) Article e2020GC009428. ISSN 1525-2027 (2020) [Refereed Article] http://ecite.utas.edu.au/143094 Engineering Fluid mechanics and thermal engineering Computational methods in fluid flow heat and mass transfer (incl. computational fluid dynamics) Refereed Article PeerReviewed 2020 ftunivtasecite https://doi.org/10.1029/2020GC009428 2022-08-29T22:18:13Z We present a refined map of geothermal heat flow for Antarctica, Aq1, based on multiple observables. The map is generated using a similarity detection approach by attributing observables from geophysics and geology to a large number of high‐quality heat flow values ( N =5,792) from other continents. Observables from global, continental, and regional datasets for Antarctica are used with a weighting function that allows the degree of similarity to increase with proximity and how similar the observables are. The similarity detection parameters are optimized through cross correlation. For each grid cell in Antarctica, a weighted average heat flow value and uncertainty metrics are calculated. The Aq1 model provides higher spatial resolution in comparison to previous results. High heat flow is shown in the Thwaites Glacier region, with local values over 150mWm −2 . We also map elevated values over 80 mWm −2 in Palmer Land, Marie Byrd Land, Victoria Land and Queen Mary Land. Very low heat flow is shown in the interior of Wilkes Land and Coats Land, with values under 40 mWm −2 . We anticipate that the new geothermal heat flow map, Aq1, and its uncertainty bounds will find extended use in providing boundary conditions for ice sheet modeling and understanding the interactions between the cryosphere and solid Earth. The computational framework and open architecture allow for the model to be reproduced, adapted and updated with additional data, or model subsets to be output at higher resolution for regional studies. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Marie Byrd Land Palmer Land Queen Mary land Thwaites Glacier Victoria Land Wilkes Land eCite UTAS (University of Tasmania) Antarctic Victoria Land Byrd Wilkes Land ENVELOPE(120.000,120.000,-69.000,-69.000) Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) Palmer Land ENVELOPE(-65.000,-65.000,-71.500,-71.500) Coats Land ENVELOPE(-27.500,-27.500,-77.000,-77.000) Queen Mary Land ENVELOPE(96.000,96.000,-68.000,-68.000) Geochemistry, Geophysics, Geosystems 22 2
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Engineering
Fluid mechanics and thermal engineering
Computational methods in fluid flow
heat and mass transfer (incl. computational fluid dynamics)
spellingShingle Engineering
Fluid mechanics and thermal engineering
Computational methods in fluid flow
heat and mass transfer (incl. computational fluid dynamics)
Staal, T
Reading, AM
Halpin, JA
Whittaker, J
Antarctic Geothermal Heat Flow Model: Aq1
topic_facet Engineering
Fluid mechanics and thermal engineering
Computational methods in fluid flow
heat and mass transfer (incl. computational fluid dynamics)
description We present a refined map of geothermal heat flow for Antarctica, Aq1, based on multiple observables. The map is generated using a similarity detection approach by attributing observables from geophysics and geology to a large number of high‐quality heat flow values ( N =5,792) from other continents. Observables from global, continental, and regional datasets for Antarctica are used with a weighting function that allows the degree of similarity to increase with proximity and how similar the observables are. The similarity detection parameters are optimized through cross correlation. For each grid cell in Antarctica, a weighted average heat flow value and uncertainty metrics are calculated. The Aq1 model provides higher spatial resolution in comparison to previous results. High heat flow is shown in the Thwaites Glacier region, with local values over 150mWm −2 . We also map elevated values over 80 mWm −2 in Palmer Land, Marie Byrd Land, Victoria Land and Queen Mary Land. Very low heat flow is shown in the interior of Wilkes Land and Coats Land, with values under 40 mWm −2 . We anticipate that the new geothermal heat flow map, Aq1, and its uncertainty bounds will find extended use in providing boundary conditions for ice sheet modeling and understanding the interactions between the cryosphere and solid Earth. The computational framework and open architecture allow for the model to be reproduced, adapted and updated with additional data, or model subsets to be output at higher resolution for regional studies.
format Article in Journal/Newspaper
author Staal, T
Reading, AM
Halpin, JA
Whittaker, J
author_facet Staal, T
Reading, AM
Halpin, JA
Whittaker, J
author_sort Staal, T
title Antarctic Geothermal Heat Flow Model: Aq1
title_short Antarctic Geothermal Heat Flow Model: Aq1
title_full Antarctic Geothermal Heat Flow Model: Aq1
title_fullStr Antarctic Geothermal Heat Flow Model: Aq1
title_full_unstemmed Antarctic Geothermal Heat Flow Model: Aq1
title_sort antarctic geothermal heat flow model: aq1
publisher Amer Geophysical Union
publishDate 2020
url https://doi.org/10.1029/2020GC009428
http://ecite.utas.edu.au/143094
long_lat ENVELOPE(120.000,120.000,-69.000,-69.000)
ENVELOPE(-130.000,-130.000,-78.000,-78.000)
ENVELOPE(-106.750,-106.750,-75.500,-75.500)
ENVELOPE(-65.000,-65.000,-71.500,-71.500)
ENVELOPE(-27.500,-27.500,-77.000,-77.000)
ENVELOPE(96.000,96.000,-68.000,-68.000)
geographic Antarctic
Victoria Land
Byrd
Wilkes Land
Marie Byrd Land
Thwaites Glacier
Palmer Land
Coats Land
Queen Mary Land
geographic_facet Antarctic
Victoria Land
Byrd
Wilkes Land
Marie Byrd Land
Thwaites Glacier
Palmer Land
Coats Land
Queen Mary Land
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Marie Byrd Land
Palmer Land
Queen Mary land
Thwaites Glacier
Victoria Land
Wilkes Land
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Marie Byrd Land
Palmer Land
Queen Mary land
Thwaites Glacier
Victoria Land
Wilkes Land
op_relation http://dx.doi.org/10.1029/2020GC009428
Staal, T and Reading, AM and Halpin, JA and Whittaker, J, Antarctic Geothermal Heat Flow Model: Aq1, Geochemistry, Geophysics, Geosystems, 22, (2) Article e2020GC009428. ISSN 1525-2027 (2020) [Refereed Article]
http://ecite.utas.edu.au/143094
op_doi https://doi.org/10.1029/2020GC009428
container_title Geochemistry, Geophysics, Geosystems
container_volume 22
container_issue 2
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