Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica.
The geothermal heat flux is one of the least well known parameters of subglacial Antarctica. Several techniques exist to obtain this essential information. However, since direct measurements are only limited to a few deep drillings to the bed, there is always a substantial amount of ice sheet and th...
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ftunivbruxelles:oai:dipot.ulb.ac.be:2013/151321 2023-05-15T13:37:29+02:00 Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. Van Liefferinge, Brice Pattyn, Frank European Geosciences Union (EGU) General Assembly 2013 (Session CR3.3/CL1.11: Ice-sheet and climate interactions. 2013-04-07/12: Vienna (Austria)) 2013-04-11 1 full-text file(s): application/pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/151321 https://dipot.ulb.ac.be/dspace/bitstream/2013/151321/1/EGU_2013_BVL.pdf en eng https://dipot.ulb.ac.be/dspace/bitstream/2013/151321/1/EGU_2013_BVL.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/151321 1 full-text file(s): info:eu-repo/semantics/openAccess Glaciologie info:eu-repo/semantics/conferencePoster info:ulb-repo/semantics/conferencePoster info:ulb-repo/semantics/openurl/document 2013 ftunivbruxelles 2022-06-12T22:09:17Z The geothermal heat flux is one of the least well known parameters of subglacial Antarctica. Several techniques exist to obtain this essential information. However, since direct measurements are only limited to a few deep drillings to the bed, there is always a substantial amount of ice sheet and thermodynamical modeling involved. This can either be done based on a fully coupled thermomechanical ice sheet model, or a thermodynamical model coupled to present-day ice sheet geometry and environmental conditions. The latter technique was recently employed by Pattyn (2010) in an attempt to determine the likelihood of basal temperate conditions of the Antarctic ice sheet using a series of existing datasets on mass balance and geothermal heat flux. Here, we present an update of this estimate using new data on bedrock elevation and ice thickness (Bedmap2; Fretwell et al. 2012) and observed surface velocities obtained from interferometric analysis (Rignot et al. 2011). The latter were further constrained by a hybrid ice sheet/ice shelf model to correct for the interior ice flow (where error of observations are to high) and for correcting the ice flow across subglacial lakes. We coupled the model with a new lake inventory from Wright et al. (in review) to improve the contribution of the geothermal heat flux to the temperature. This revised calculation of the temperature allows us to improve our knowledge of basal melting.We determined different areas with a high likelihood to find million year-old ice, further constrained by low horizontal flow velocities and relative thick ice to ensure a straightforward climatic signal over such long period of time. info:eu-repo/semantics/nonPublished Conference Object Antarc* Antarctic Antarctica Ice Sheet Ice Shelf DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) Antarctic New Lake ENVELOPE(-109.468,-109.468,62.684,62.684) The Antarctic |
institution |
Open Polar |
collection |
DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
op_collection_id |
ftunivbruxelles |
language |
English |
topic |
Glaciologie |
spellingShingle |
Glaciologie Van Liefferinge, Brice Pattyn, Frank Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
topic_facet |
Glaciologie |
description |
The geothermal heat flux is one of the least well known parameters of subglacial Antarctica. Several techniques exist to obtain this essential information. However, since direct measurements are only limited to a few deep drillings to the bed, there is always a substantial amount of ice sheet and thermodynamical modeling involved. This can either be done based on a fully coupled thermomechanical ice sheet model, or a thermodynamical model coupled to present-day ice sheet geometry and environmental conditions. The latter technique was recently employed by Pattyn (2010) in an attempt to determine the likelihood of basal temperate conditions of the Antarctic ice sheet using a series of existing datasets on mass balance and geothermal heat flux. Here, we present an update of this estimate using new data on bedrock elevation and ice thickness (Bedmap2; Fretwell et al. 2012) and observed surface velocities obtained from interferometric analysis (Rignot et al. 2011). The latter were further constrained by a hybrid ice sheet/ice shelf model to correct for the interior ice flow (where error of observations are to high) and for correcting the ice flow across subglacial lakes. We coupled the model with a new lake inventory from Wright et al. (in review) to improve the contribution of the geothermal heat flux to the temperature. This revised calculation of the temperature allows us to improve our knowledge of basal melting.We determined different areas with a high likelihood to find million year-old ice, further constrained by low horizontal flow velocities and relative thick ice to ensure a straightforward climatic signal over such long period of time. info:eu-repo/semantics/nonPublished |
author2 |
European Geosciences Union (EGU) General Assembly 2013 (Session CR3.3/CL1.11: Ice-sheet and climate interactions. 2013-04-07/12: Vienna (Austria)) |
format |
Conference Object |
author |
Van Liefferinge, Brice Pattyn, Frank |
author_facet |
Van Liefferinge, Brice Pattyn, Frank |
author_sort |
Van Liefferinge, Brice |
title |
Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
title_short |
Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
title_full |
Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
title_fullStr |
Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
title_full_unstemmed |
Geothermal heat flux uncertainties and the search for million year-old ice in Antarctica. |
title_sort |
geothermal heat flux uncertainties and the search for million year-old ice in antarctica. |
publishDate |
2013 |
url |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/151321 https://dipot.ulb.ac.be/dspace/bitstream/2013/151321/1/EGU_2013_BVL.pdf |
long_lat |
ENVELOPE(-109.468,-109.468,62.684,62.684) |
geographic |
Antarctic New Lake The Antarctic |
geographic_facet |
Antarctic New Lake The Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf |
op_relation |
https://dipot.ulb.ac.be/dspace/bitstream/2013/151321/1/EGU_2013_BVL.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/151321 |
op_rights |
1 full-text file(s): info:eu-repo/semantics/openAccess |
_version_ |
1766092498484068352 |