Combining upper crust and lithosphere contributions to heat flow models
Geothermal heat supplied to the base of Antarctic ice sheets, and the spatial variation of supplied heat, is animportant input model parameter in ice sheet models. Continental models of heat flow (usually referred to inthe cryosphere research community as heat flux density, abbreviated to heat flux)...
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ftunivtasecite:oai:ecite.utas.edu.au:131210 2023-05-15T13:55:18+02:00 Combining upper crust and lithosphere contributions to heat flow models Reading, A Staal, T Halpin, J Whittaker, J 2018 application/pdf https://www.polar2018.org/ http://ecite.utas.edu.au/131210 en eng . http://ecite.utas.edu.au/131210/1/polar2018_abstractproceedings 2479.pdf Reading, A and Staal, T and Halpin, J and Whittaker, J, Combining upper crust and lithosphere contributions to heat flow models, POLAR2018 Open Science Conference Abstract Proceedings, 19-23 June 2018, Davos, Switzerland, pp. 2479. (2018) [Conference Extract] http://ecite.utas.edu.au/131210 Earth Sciences Geophysics Geodynamics Conference Extract NonPeerReviewed 2018 ftunivtasecite 2019-12-13T22:29:08Z Geothermal heat supplied to the base of Antarctic ice sheets, and the spatial variation of supplied heat, is animportant input model parameter in ice sheet models. Continental models of heat flow (usually referred to inthe cryosphere research community as heat flux density, abbreviated to heat flux) may be generated usingseismic wavespeed tomography maps or by inference from other geophysical observables. Upper crustalmodels, however, are generated directly from measuring the heat production of dominant or particularlyradiogenic lithologies.In this contribution, we combine upper crust and lithosphere contributions to heat flow models with a focus onEast Antarctica, including the continental interior which is covered by ice of several kilometres thickness. Wereview alternative approaches to combining low resolution information on the deeper lithosphere with broadspatial coverage, and high resolution information with very limited spatial coverage relating to the uppercrustal. Providing effective estimates of the heat supplied by the upper crust is an important research goal dueto the significance of small pockets of elevated heat flow on ice sheet models. Our model for East Antarcticarepresents a step towards future probabilistic approaches to solid Earth constraints for ice sheet models. Conference Object Antarc* Antarctic Antarctica Ice Sheet eCite UTAS (University of Tasmania) Antarctic |
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Open Polar |
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eCite UTAS (University of Tasmania) |
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ftunivtasecite |
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English |
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Earth Sciences Geophysics Geodynamics |
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Earth Sciences Geophysics Geodynamics Reading, A Staal, T Halpin, J Whittaker, J Combining upper crust and lithosphere contributions to heat flow models |
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Earth Sciences Geophysics Geodynamics |
description |
Geothermal heat supplied to the base of Antarctic ice sheets, and the spatial variation of supplied heat, is animportant input model parameter in ice sheet models. Continental models of heat flow (usually referred to inthe cryosphere research community as heat flux density, abbreviated to heat flux) may be generated usingseismic wavespeed tomography maps or by inference from other geophysical observables. Upper crustalmodels, however, are generated directly from measuring the heat production of dominant or particularlyradiogenic lithologies.In this contribution, we combine upper crust and lithosphere contributions to heat flow models with a focus onEast Antarctica, including the continental interior which is covered by ice of several kilometres thickness. Wereview alternative approaches to combining low resolution information on the deeper lithosphere with broadspatial coverage, and high resolution information with very limited spatial coverage relating to the uppercrustal. Providing effective estimates of the heat supplied by the upper crust is an important research goal dueto the significance of small pockets of elevated heat flow on ice sheet models. Our model for East Antarcticarepresents a step towards future probabilistic approaches to solid Earth constraints for ice sheet models. |
format |
Conference Object |
author |
Reading, A Staal, T Halpin, J Whittaker, J |
author_facet |
Reading, A Staal, T Halpin, J Whittaker, J |
author_sort |
Reading, A |
title |
Combining upper crust and lithosphere contributions to heat flow models |
title_short |
Combining upper crust and lithosphere contributions to heat flow models |
title_full |
Combining upper crust and lithosphere contributions to heat flow models |
title_fullStr |
Combining upper crust and lithosphere contributions to heat flow models |
title_full_unstemmed |
Combining upper crust and lithosphere contributions to heat flow models |
title_sort |
combining upper crust and lithosphere contributions to heat flow models |
publisher |
. |
publishDate |
2018 |
url |
https://www.polar2018.org/ http://ecite.utas.edu.au/131210 |
geographic |
Antarctic |
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Antarctic |
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Antarc* Antarctic Antarctica Ice Sheet |
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Antarc* Antarctic Antarctica Ice Sheet |
op_relation |
http://ecite.utas.edu.au/131210/1/polar2018_abstractproceedings 2479.pdf Reading, A and Staal, T and Halpin, J and Whittaker, J, Combining upper crust and lithosphere contributions to heat flow models, POLAR2018 Open Science Conference Abstract Proceedings, 19-23 June 2018, Davos, Switzerland, pp. 2479. (2018) [Conference Extract] http://ecite.utas.edu.au/131210 |
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