Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate
The mid-Holocene (MH) is the most recent typical climate period and a subject of great interest in global paleocultural research. Following the latest Paleoclimate Modeling Intercomparison Project phase 4 (PMIP4) protocol and using a fully coupled climate model, we simulated the climate during both...
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ftcopernicus:oai:publications.copernicus.org:cp109962 2023-11-12T04:22:34+01:00 Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate Kang, Yibo Yang, Haijun 2023-10-24 application/pdf https://doi.org/10.5194/cp-19-2013-2023 https://cp.copernicus.org/articles/19/2013/2023/ eng eng doi:10.5194/cp-19-2013-2023 https://cp.copernicus.org/articles/19/2013/2023/ eISSN: 1814-9332 Text 2023 ftcopernicus https://doi.org/10.5194/cp-19-2013-2023 2023-10-30T17:24:16Z The mid-Holocene (MH) is the most recent typical climate period and a subject of great interest in global paleocultural research. Following the latest Paleoclimate Modeling Intercomparison Project phase 4 (PMIP4) protocol and using a fully coupled climate model, we simulated the climate during both the MH and the preindustrial (PI) periods and quantified the effects of Earth orbital parameters (ORBs) and greenhouse gases (GHGs) on climate differences, focusing on the simulated differences in the Atlantic meridional overturning circulation (AMOC) between these two periods. Compared to the PI simulation, the ORB effect in the MH simulation led to seasonal enhancement of temperature, consistent with previous findings. In the MH simulation, the ORB effect led to a markedly warmer climate in the mid–high latitudes and increased precipitation in the Northern Hemisphere, which were partially offset by the cooling effect of the lower GHGs. The AMOC in the MH simulation was about 4 % stronger than that in the PI simulation. The ORB effect led to 6 % enhancement of the AMOC in the MH simulation, which was, however, partly neutralized by the GHG effect. Transient simulation from the MH to the PI further demonstrated the opposite effects of ORBs and GHGs on the evolution of the AMOC during the past 6000 years. The simulated stronger AMOC in the MH was mainly due to the thinner sea ice in the polar oceans caused by the ORB effect, which reduced the freshwater flux export to the subpolar Atlantic and resulted in a more saline North Atlantic. This study may help us quantitatively understand the roles of different external forcing factors in Earth's climate evolution since the MH. Text North Atlantic Sea ice Copernicus Publications: E-Journals Climate of the Past 19 10 2013 2026 |
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Copernicus Publications: E-Journals |
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English |
description |
The mid-Holocene (MH) is the most recent typical climate period and a subject of great interest in global paleocultural research. Following the latest Paleoclimate Modeling Intercomparison Project phase 4 (PMIP4) protocol and using a fully coupled climate model, we simulated the climate during both the MH and the preindustrial (PI) periods and quantified the effects of Earth orbital parameters (ORBs) and greenhouse gases (GHGs) on climate differences, focusing on the simulated differences in the Atlantic meridional overturning circulation (AMOC) between these two periods. Compared to the PI simulation, the ORB effect in the MH simulation led to seasonal enhancement of temperature, consistent with previous findings. In the MH simulation, the ORB effect led to a markedly warmer climate in the mid–high latitudes and increased precipitation in the Northern Hemisphere, which were partially offset by the cooling effect of the lower GHGs. The AMOC in the MH simulation was about 4 % stronger than that in the PI simulation. The ORB effect led to 6 % enhancement of the AMOC in the MH simulation, which was, however, partly neutralized by the GHG effect. Transient simulation from the MH to the PI further demonstrated the opposite effects of ORBs and GHGs on the evolution of the AMOC during the past 6000 years. The simulated stronger AMOC in the MH was mainly due to the thinner sea ice in the polar oceans caused by the ORB effect, which reduced the freshwater flux export to the subpolar Atlantic and resulted in a more saline North Atlantic. This study may help us quantitatively understand the roles of different external forcing factors in Earth's climate evolution since the MH. |
format |
Text |
author |
Kang, Yibo Yang, Haijun |
spellingShingle |
Kang, Yibo Yang, Haijun Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
author_facet |
Kang, Yibo Yang, Haijun |
author_sort |
Kang, Yibo |
title |
Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
title_short |
Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
title_full |
Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
title_fullStr |
Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
title_full_unstemmed |
Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate |
title_sort |
quantifying effects of earth orbital parameters and greenhouse gases on mid-holocene climate |
publishDate |
2023 |
url |
https://doi.org/10.5194/cp-19-2013-2023 https://cp.copernicus.org/articles/19/2013/2023/ |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-19-2013-2023 https://cp.copernicus.org/articles/19/2013/2023/ |
op_doi |
https://doi.org/10.5194/cp-19-2013-2023 |
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Climate of the Past |
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19 |
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10 |
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2013 |
op_container_end_page |
2026 |
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1782337588024049664 |