The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials
The response of the climate system to astronomical parameters, greenhouse gases (GHG) and ice sheets is an important scientific issue, but the regional difference need to be better understood, including the forcing mechanisms, internal processes and feedbacks. Based on the numerical simulations duri...
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ftunivlouvain:oai:dial.uclouvain.be:boreal:268993 2024-05-12T07:59:39+00:00 The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials Wu, Zhipeng Yin, Qiuzhen Guo, Zhengtang Berger, André Belgian National Comittee for Geodesy and Geophysics study day UCL - SST/ELI - Earth and Life Institute UCL - SST/ELI/ELIC - Earth & Climate 2022 http://hdl.handle.net/2078.1/268993 eng eng info:eu-repo/grantAgreement/Université catholique de Louvain/MIS/QuantLoess boreal:268993 http://hdl.handle.net/2078.1/268993 info:eu-repo/semantics/openAccess info:eu-repo/semantics/conferenceObject 2022 ftunivlouvain 2024-04-17T16:32:11Z The response of the climate system to astronomical parameters, greenhouse gases (GHG) and ice sheets is an important scientific issue, but the regional difference need to be better understood, including the forcing mechanisms, internal processes and feedbacks. Based on the numerical simulations during past interglacials using the model LOVECLIM, we investigate the different response of the sea ice and sea surface temperature (SST) to astronomical parameters, GHG and ice sheets at different regions. Our results show that the Arctic sea ice variation is primarily controlled by local summer insolation, while the Southern Ocean sea ice variation is more influenced by the CO2 concentration but the effect of local summer insolation can’t be ignored. In terms of the astronomical parameters, precession plays a dominant role on the Arctic sea ice, while obliquity plays a dominant role on the Southern Ocean sea ice. As far as the SST is concerned, it shows a strong precessional signal at low latitudes in both hemispheres. For the SST in the mid and high latitudes, obliquity plays a dominant role in the SH whereas precession is more important in the NH. The internal processes and feedbacks will be given in detail in the presentation. In addition, the different response of the sea ice and SST to GHG and ice sheets based on the transient simulations will be investigated in the future study. Conference Object Arctic Sea ice Southern Ocean DIAL@UCLouvain (Université catholique de Louvain) Arctic Southern Ocean |
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Open Polar |
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DIAL@UCLouvain (Université catholique de Louvain) |
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ftunivlouvain |
language |
English |
description |
The response of the climate system to astronomical parameters, greenhouse gases (GHG) and ice sheets is an important scientific issue, but the regional difference need to be better understood, including the forcing mechanisms, internal processes and feedbacks. Based on the numerical simulations during past interglacials using the model LOVECLIM, we investigate the different response of the sea ice and sea surface temperature (SST) to astronomical parameters, GHG and ice sheets at different regions. Our results show that the Arctic sea ice variation is primarily controlled by local summer insolation, while the Southern Ocean sea ice variation is more influenced by the CO2 concentration but the effect of local summer insolation can’t be ignored. In terms of the astronomical parameters, precession plays a dominant role on the Arctic sea ice, while obliquity plays a dominant role on the Southern Ocean sea ice. As far as the SST is concerned, it shows a strong precessional signal at low latitudes in both hemispheres. For the SST in the mid and high latitudes, obliquity plays a dominant role in the SH whereas precession is more important in the NH. The internal processes and feedbacks will be given in detail in the presentation. In addition, the different response of the sea ice and SST to GHG and ice sheets based on the transient simulations will be investigated in the future study. |
author2 |
UCL - SST/ELI - Earth and Life Institute UCL - SST/ELI/ELIC - Earth & Climate |
format |
Conference Object |
author |
Wu, Zhipeng Yin, Qiuzhen Guo, Zhengtang Berger, André Belgian National Comittee for Geodesy and Geophysics study day |
spellingShingle |
Wu, Zhipeng Yin, Qiuzhen Guo, Zhengtang Berger, André Belgian National Comittee for Geodesy and Geophysics study day The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
author_facet |
Wu, Zhipeng Yin, Qiuzhen Guo, Zhengtang Berger, André Belgian National Comittee for Geodesy and Geophysics study day |
author_sort |
Wu, Zhipeng |
title |
The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
title_short |
The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
title_full |
The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
title_fullStr |
The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
title_full_unstemmed |
The different response of the climate system to astronomical parameters, GHG and ice sheets during past interglacials |
title_sort |
different response of the climate system to astronomical parameters, ghg and ice sheets during past interglacials |
publishDate |
2022 |
url |
http://hdl.handle.net/2078.1/268993 |
geographic |
Arctic Southern Ocean |
geographic_facet |
Arctic Southern Ocean |
genre |
Arctic Sea ice Southern Ocean |
genre_facet |
Arctic Sea ice Southern Ocean |
op_relation |
info:eu-repo/grantAgreement/Université catholique de Louvain/MIS/QuantLoess boreal:268993 http://hdl.handle.net/2078.1/268993 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1798841229175160832 |