A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions
The excess freshwater in the Arctic due to global warming is causing a weakening the Atlantic Meridional Overturning Circulation (AMOC). The question of how the climate change will impact the stability of the AMOC, however, remains unclear. We address this uncertainty through a series of ensemble si...
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:281764 2024-05-12T08:00:08+00:00 A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions Liu, Wei Shi, Feng Zhang, Xiao Xue, Huihong Yin, Qiuzhen 21st Congress of the International Union for Quaternary Research (INQUA) UCL - SST/ELI/ELIC - Earth & Climate 2023 http://hdl.handle.net/2078.1/281764 eng eng info:eu-repo/grantAgreement/FRS-FNRS/PDR/FNRS T.0246.23 boreal:281764 http://hdl.handle.net/2078.1/281764 Atlantic Meridional Overturning Circulation Freshwater hosing Hysteresis Future warming info:eu-repo/semantics/conferenceObject 2023 ftunistlouisbrus 2024-04-18T16:58:15Z The excess freshwater in the Arctic due to global warming is causing a weakening the Atlantic Meridional Overturning Circulation (AMOC). The question of how the climate change will impact the stability of the AMOC, however, remains unclear. We address this uncertainty through a series of ensemble simulations (100 members) using freshwater hysteresis experiments, aiming to elucidate potential changes in AMOC stability across different interglacials. Our findings suggest that future increases in anthropogenic CO2 emissions will bolster the AMOC's resistance to excess freshwater, though it exhibits less resilience compared to past interglacials. In future climate scenarios, warmer conditions lead to a notable delay in sea ice expansion, which aids in the preservation of deep water formation and AMOC strength. Concurrently, an intensification of freshwater convergence in the North Atlantic acts as a dampening factor during AMOC recovery under warmer climate background. The influence of orbital parameters on AMOC stability across different interglacialods is found to be relatively minor. These results underscore the importance of considering background climate conditions, particularly CO2 concentrations, when investigating future AMOC changes and making comparisons to past AMOC dynamics. Conference Object Arctic Climate change Global warming North Atlantic Sea ice DIAL@USL-B (Université Saint-Louis, Bruxelles) Arctic |
institution |
Open Polar |
collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
op_collection_id |
ftunistlouisbrus |
language |
English |
topic |
Atlantic Meridional Overturning Circulation Freshwater hosing Hysteresis Future warming |
spellingShingle |
Atlantic Meridional Overturning Circulation Freshwater hosing Hysteresis Future warming Liu, Wei Shi, Feng Zhang, Xiao Xue, Huihong Yin, Qiuzhen 21st Congress of the International Union for Quaternary Research (INQUA) A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
topic_facet |
Atlantic Meridional Overturning Circulation Freshwater hosing Hysteresis Future warming |
description |
The excess freshwater in the Arctic due to global warming is causing a weakening the Atlantic Meridional Overturning Circulation (AMOC). The question of how the climate change will impact the stability of the AMOC, however, remains unclear. We address this uncertainty through a series of ensemble simulations (100 members) using freshwater hysteresis experiments, aiming to elucidate potential changes in AMOC stability across different interglacials. Our findings suggest that future increases in anthropogenic CO2 emissions will bolster the AMOC's resistance to excess freshwater, though it exhibits less resilience compared to past interglacials. In future climate scenarios, warmer conditions lead to a notable delay in sea ice expansion, which aids in the preservation of deep water formation and AMOC strength. Concurrently, an intensification of freshwater convergence in the North Atlantic acts as a dampening factor during AMOC recovery under warmer climate background. The influence of orbital parameters on AMOC stability across different interglacialods is found to be relatively minor. These results underscore the importance of considering background climate conditions, particularly CO2 concentrations, when investigating future AMOC changes and making comparisons to past AMOC dynamics. |
author2 |
UCL - SST/ELI/ELIC - Earth & Climate |
format |
Conference Object |
author |
Liu, Wei Shi, Feng Zhang, Xiao Xue, Huihong Yin, Qiuzhen 21st Congress of the International Union for Quaternary Research (INQUA) |
author_facet |
Liu, Wei Shi, Feng Zhang, Xiao Xue, Huihong Yin, Qiuzhen 21st Congress of the International Union for Quaternary Research (INQUA) |
author_sort |
Liu, Wei |
title |
A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
title_short |
A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
title_full |
A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
title_fullStr |
A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
title_full_unstemmed |
A threshold in the collapse and recovery of Atlantic Meridional Overturning Circulation in response to different interglacial conditions |
title_sort |
threshold in the collapse and recovery of atlantic meridional overturning circulation in response to different interglacial conditions |
publishDate |
2023 |
url |
http://hdl.handle.net/2078.1/281764 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Global warming North Atlantic Sea ice |
genre_facet |
Arctic Climate change Global warming North Atlantic Sea ice |
op_relation |
info:eu-repo/grantAgreement/FRS-FNRS/PDR/FNRS T.0246.23 boreal:281764 http://hdl.handle.net/2078.1/281764 |
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1798841866281549824 |