Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica.
Antarctic mass balance is mainly controlled by surface mass balance (SMB, i.e. the net effect of precipitations at the surface of the ice sheet) and ice discharge at its margins, mostly through ice shelves. These floating ice bodies made from ice flowing from the continent to the ocean are buttresse...
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Other Authors: | , , , , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
Published: |
Universite Libre de Bruxelles
2017
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Subjects: | |
Online Access: | http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/254506 https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/5/ThesisManuscriptEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/7/Appendix.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/8/ContratDiPhilippe.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/3/Contents.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/6/ThesisManuscriptNoEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/4/Appendix2.pdf |
id |
ftunivbruxelles:oai:dipot.ulb.ac.be:2013/254506 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
op_collection_id |
ftunivbruxelles |
language |
English |
topic |
Glaciologie Ice core surface mass balance accumulation vertical strain rate density Antarctica |
spellingShingle |
Glaciologie Ice core surface mass balance accumulation vertical strain rate density Antarctica Philippe, Morgane Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
topic_facet |
Glaciologie Ice core surface mass balance accumulation vertical strain rate density Antarctica |
description |
Antarctic mass balance is mainly controlled by surface mass balance (SMB, i.e. the net effect of precipitations at the surface of the ice sheet) and ice discharge at its margins, mostly through ice shelves. These floating ice bodies made from ice flowing from the continent to the ocean are buttressed by ice rises (elevation of the sea floor on which ice shelf re-grounds) such as the Derwael Ice Rise (DIR) in Dronning Maud Land (DML). In addition to this role important to consider in the future contribution of Antarctica to sea level rise, ice rises are also “climate dipsticks” helping to reconstruct the climate of the past centuries to millennia at high resolution. Due to their coastal location, they witness the changes happening there more rapidly than inland. Furthermore, their internal stratigraphy forms arches that allow to assess their stability, to date their own formation and therefore, in some cases, to constrain the past extension of the ice sheet at the scale of several millennia. As part of the IceCon project :Constraining ice mass changes in Antarctica, this thesis aimed to drill a 120 m ice core (named IC12 for the IceCon project, 2012) at the divide of the DIR and perform physico-chemical analyses to study its density and its internal annual layering with the aim of reconstructing SMB of the last two centuries. We also recorded a virtual image of the borehole using an optical televiewer (OPTV) to assess the ability of this instrument to reconstruct a density profile and measure vertical strain rates when the logging is repeated in the same borehole after a sufficient period of time (here, 2 years).The results show a general increase in snow accumulation rates (SMB) of 30-40% during the 20th century, particularly marked during the last 20-50 years. SMB variability is governed to a large extent by atmospheric circulation and to a lesser extent by variations in sea ice cover. The vertical velocity profile measured from repeat borehole OPTV was applied to refine SMB correction and the results fall in ... |
author2 |
Tison, Jean-Louis Pattyn, Frank Debaille, Vinciane Hubbard, Bryn Dehairs, Frank |
format |
Doctoral or Postdoctoral Thesis |
author |
Philippe, Morgane |
author_facet |
Philippe, Morgane |
author_sort |
Philippe, Morgane |
title |
Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
title_short |
Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
title_full |
Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
title_fullStr |
Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
title_full_unstemmed |
Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. |
title_sort |
reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the derwael ice rise in coastal dronning maud land, east antarctica. |
publisher |
Universite Libre de Bruxelles |
publishDate |
2017 |
url |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/254506 https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/5/ThesisManuscriptEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/7/Appendix.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/8/ContratDiPhilippe.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/3/Contents.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/6/ThesisManuscriptNoEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/4/Appendix2.pdf |
geographic |
Antarctic East Antarctica Dronning Maud Land |
geographic_facet |
Antarctic East Antarctica Dronning Maud Land |
genre |
Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica ice core Ice Sheet Ice Shelf Ice Shelves Sea ice |
genre_facet |
Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica ice core Ice Sheet Ice Shelf Ice Shelves Sea ice |
op_relation |
https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/5/ThesisManuscriptEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/7/Appendix.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/8/ContratDiPhilippe.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/3/Contents.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/6/ThesisManuscriptNoEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/4/Appendix2.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/254506 |
op_rights |
6 full-text file(s): info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/closedAccess | info:eu-repo/semantics/openAccess | info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/restrictedAccess |
_version_ |
1766092595012829184 |
spelling |
ftunivbruxelles:oai:dipot.ulb.ac.be:2013/254506 2023-05-15T13:37:30+02:00 Reconstruction of the density profile, surface mass balance history and vertical strain profile on the divide of the Derwael Ice Rise in coastal Dronning Maud Land, East Antarctica. Philippe, Morgane Tison, Jean-Louis Pattyn, Frank Debaille, Vinciane Hubbard, Bryn Dehairs, Frank 2017-07-06 6 full-text file(s): application/pdf | application/pdf | application/pdf | application/pdf | application/pdf | application/pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/254506 https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/5/ThesisManuscriptEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/7/Appendix.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/8/ContratDiPhilippe.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/3/Contents.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/6/ThesisManuscriptNoEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/4/Appendix2.pdf en eng Universite Libre de Bruxelles Université libre de Bruxelles, Faculté des Sciences – Sciences de la Terre et de l'Environnement, Bruxelles https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/5/ThesisManuscriptEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/7/Appendix.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/8/ContratDiPhilippe.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/3/Contents.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/6/ThesisManuscriptNoEmbargo.pdf https://dipot.ulb.ac.be/dspace/bitstream/2013/254506/4/Appendix2.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/254506 6 full-text file(s): info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/closedAccess | info:eu-repo/semantics/openAccess | info:eu-repo/semantics/restrictedAccess | info:eu-repo/semantics/restrictedAccess Glaciologie Ice core surface mass balance accumulation vertical strain rate density Antarctica info:eu-repo/semantics/doctoralThesis info:ulb-repo/semantics/doctoralThesis info:ulb-repo/semantics/openurl/vlink-dissertation 2017 ftunivbruxelles 2022-06-12T22:09:21Z Antarctic mass balance is mainly controlled by surface mass balance (SMB, i.e. the net effect of precipitations at the surface of the ice sheet) and ice discharge at its margins, mostly through ice shelves. These floating ice bodies made from ice flowing from the continent to the ocean are buttressed by ice rises (elevation of the sea floor on which ice shelf re-grounds) such as the Derwael Ice Rise (DIR) in Dronning Maud Land (DML). In addition to this role important to consider in the future contribution of Antarctica to sea level rise, ice rises are also “climate dipsticks” helping to reconstruct the climate of the past centuries to millennia at high resolution. Due to their coastal location, they witness the changes happening there more rapidly than inland. Furthermore, their internal stratigraphy forms arches that allow to assess their stability, to date their own formation and therefore, in some cases, to constrain the past extension of the ice sheet at the scale of several millennia. As part of the IceCon project :Constraining ice mass changes in Antarctica, this thesis aimed to drill a 120 m ice core (named IC12 for the IceCon project, 2012) at the divide of the DIR and perform physico-chemical analyses to study its density and its internal annual layering with the aim of reconstructing SMB of the last two centuries. We also recorded a virtual image of the borehole using an optical televiewer (OPTV) to assess the ability of this instrument to reconstruct a density profile and measure vertical strain rates when the logging is repeated in the same borehole after a sufficient period of time (here, 2 years).The results show a general increase in snow accumulation rates (SMB) of 30-40% during the 20th century, particularly marked during the last 20-50 years. SMB variability is governed to a large extent by atmospheric circulation and to a lesser extent by variations in sea ice cover. The vertical velocity profile measured from repeat borehole OPTV was applied to refine SMB correction and the results fall in ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica DML Dronning Maud Land East Antarctica ice core Ice Sheet Ice Shelf Ice Shelves Sea ice DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) Antarctic East Antarctica Dronning Maud Land |