Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia
The climate variability at multi-decadal and centennial scale over Antarctica is closely linked to the stability of regional glaciers, the whole ice sheet mass balance, and thus the estimation of future sea-level rise. However, the short instrumental data limit our ability to fully estimate such low...
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:270474 2024-05-12T07:54:43+00:00 Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia Lyu, Zhiqiang UCL - SST/ELI - Earth and Life Institute UCL - Faculty of Sciences Goosse, Hugues Mahillon, Jacques Fichefet, Thierry Yin, Qiuzhen Swingedouw, Didier Thomas, Liz 2022 http://hdl.handle.net/2078.1/270474 eng eng boreal:270474 http://hdl.handle.net/2078.1/270474 info:eu-repo/semantics/openAccess Antarctica Data assimilation Past two millennia info:eu-repo/semantics/doctoralThesis 2022 ftunistlouisbrus 2024-04-18T17:09:15Z The climate variability at multi-decadal and centennial scale over Antarctica is closely linked to the stability of regional glaciers, the whole ice sheet mass balance, and thus the estimation of future sea-level rise. However, the short instrumental data limit our ability to fully estimate such low-frequency variability. The main objective of this thesis is to reconstruct the centennial variability of the Antarctic surface air temperature over the past two millennia and to understand the related physical processes by combining low and high-frequency records with climate model results using data assimilation. Our reconstruction indicates the long-term cooling over the past millennium and its spatial pattern over West Antarctica, which has been captured by the current simulations with climate models. The centennial variability of surface air temperature could be primarily linked to external forcings, for instance the volcanism, over the past millennium. In contrast, over the first millennium, natural internal variability in the climate system plays a dominant role in these low-frequency changes. Our work also highlights that data assimilation is able to achieve the combination of the low-resolution proxy records with the high frequency ones based on climate model results without assuming a stationary relationship between proxy records and the target reconstruction. The corresponding reconstruction confirms the compatible information among various sources and provides the estimation for multiple climate variables which could help us understand the relevant mechanisms that might be responsible for the origin of the proxy records. (SC - Sciences) -- UCL, 2022 Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica Ice Sheet West Antarctica DIAL@USL-B (Université Saint-Louis, Bruxelles) Antarctic The Antarctic West Antarctica |
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Open Polar |
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DIAL@USL-B (Université Saint-Louis, Bruxelles) |
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ftunistlouisbrus |
language |
English |
topic |
Antarctica Data assimilation Past two millennia |
spellingShingle |
Antarctica Data assimilation Past two millennia Lyu, Zhiqiang Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
topic_facet |
Antarctica Data assimilation Past two millennia |
description |
The climate variability at multi-decadal and centennial scale over Antarctica is closely linked to the stability of regional glaciers, the whole ice sheet mass balance, and thus the estimation of future sea-level rise. However, the short instrumental data limit our ability to fully estimate such low-frequency variability. The main objective of this thesis is to reconstruct the centennial variability of the Antarctic surface air temperature over the past two millennia and to understand the related physical processes by combining low and high-frequency records with climate model results using data assimilation. Our reconstruction indicates the long-term cooling over the past millennium and its spatial pattern over West Antarctica, which has been captured by the current simulations with climate models. The centennial variability of surface air temperature could be primarily linked to external forcings, for instance the volcanism, over the past millennium. In contrast, over the first millennium, natural internal variability in the climate system plays a dominant role in these low-frequency changes. Our work also highlights that data assimilation is able to achieve the combination of the low-resolution proxy records with the high frequency ones based on climate model results without assuming a stationary relationship between proxy records and the target reconstruction. The corresponding reconstruction confirms the compatible information among various sources and provides the estimation for multiple climate variables which could help us understand the relevant mechanisms that might be responsible for the origin of the proxy records. (SC - Sciences) -- UCL, 2022 |
author2 |
UCL - SST/ELI - Earth and Life Institute UCL - Faculty of Sciences Goosse, Hugues Mahillon, Jacques Fichefet, Thierry Yin, Qiuzhen Swingedouw, Didier Thomas, Liz |
format |
Doctoral or Postdoctoral Thesis |
author |
Lyu, Zhiqiang |
author_facet |
Lyu, Zhiqiang |
author_sort |
Lyu, Zhiqiang |
title |
Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
title_short |
Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
title_full |
Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
title_fullStr |
Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
title_full_unstemmed |
Combining climate models with high- and low-resolution proxy records to reconstruct the Antarctic centennial temperature variability over the past two millennia |
title_sort |
combining climate models with high- and low-resolution proxy records to reconstruct the antarctic centennial temperature variability over the past two millennia |
publishDate |
2022 |
url |
http://hdl.handle.net/2078.1/270474 |
geographic |
Antarctic The Antarctic West Antarctica |
geographic_facet |
Antarctic The Antarctic West Antarctica |
genre |
Antarc* Antarctic Antarctica Ice Sheet West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet West Antarctica |
op_relation |
boreal:270474 http://hdl.handle.net/2078.1/270474 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1798851675926036480 |