Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model
Abstract This paper investigates the causation for the decline of the Atlantic Meridional Overturning Circulation (AMOC) from approximately 17 Sv to about 9 Sv, when the atmospheric resolution of the Max Planck Institute‐Earth System Model is enhanced from ∼1° to ∼0.5°. The results show that the slo...
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American Geophysical Union (AGU)
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ftdoajarticles:oai:doaj.org/article:84cb4697dc2d4e0aa9e1b100733b867f 2023-05-15T17:33:25+02:00 Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model D. A. Putrasahan K. Lohmann J.‐S. vonStorch J. H. Jungclaus O. Gutjahr H. Haak 2019-05-01T00:00:00Z https://doi.org/10.1029/2018MS001447 https://doaj.org/article/84cb4697dc2d4e0aa9e1b100733b867f EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2018MS001447 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2018MS001447 https://doaj.org/article/84cb4697dc2d4e0aa9e1b100733b867f Journal of Advances in Modeling Earth Systems, Vol 11, Iss 5, Pp 1349-1363 (2019) Atlantic Meridional Overturning Circulation Wind stress effect high‐resolution global coupled climate model flux correction in a coupled system Physical geography GB3-5030 Oceanography GC1-1581 article 2019 ftdoajarticles https://doi.org/10.1029/2018MS001447 2022-12-30T20:56:59Z Abstract This paper investigates the causation for the decline of the Atlantic Meridional Overturning Circulation (AMOC) from approximately 17 Sv to about 9 Sv, when the atmospheric resolution of the Max Planck Institute‐Earth System Model is enhanced from ∼1° to ∼0.5°. The results show that the slowdown of the AMOC is caused by the cessation of deep convection. In most modeling studies, this is thought to be controlled by buoyancy fluxes in the convective regions, for example, by surface freshwater flux that is introduced locally or via enormous input from glacier or iceberg melts. While we find that freshwater is still the key to the reduction of AMOC seen in the higher‐resolution run, the freshening of the North Atlantic does not need to be directly caused by local freshwater fluxes. Instead, it can be caused indirectly through winds via a reduced wind‐driven gyre circulation and salinity transport associated to this circulation, as seen in the higher‐resolution run. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Journal of Advances in Modeling Earth Systems 11 5 1349 1363 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Atlantic Meridional Overturning Circulation Wind stress effect high‐resolution global coupled climate model flux correction in a coupled system Physical geography GB3-5030 Oceanography GC1-1581 |
spellingShingle |
Atlantic Meridional Overturning Circulation Wind stress effect high‐resolution global coupled climate model flux correction in a coupled system Physical geography GB3-5030 Oceanography GC1-1581 D. A. Putrasahan K. Lohmann J.‐S. vonStorch J. H. Jungclaus O. Gutjahr H. Haak Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
topic_facet |
Atlantic Meridional Overturning Circulation Wind stress effect high‐resolution global coupled climate model flux correction in a coupled system Physical geography GB3-5030 Oceanography GC1-1581 |
description |
Abstract This paper investigates the causation for the decline of the Atlantic Meridional Overturning Circulation (AMOC) from approximately 17 Sv to about 9 Sv, when the atmospheric resolution of the Max Planck Institute‐Earth System Model is enhanced from ∼1° to ∼0.5°. The results show that the slowdown of the AMOC is caused by the cessation of deep convection. In most modeling studies, this is thought to be controlled by buoyancy fluxes in the convective regions, for example, by surface freshwater flux that is introduced locally or via enormous input from glacier or iceberg melts. While we find that freshwater is still the key to the reduction of AMOC seen in the higher‐resolution run, the freshening of the North Atlantic does not need to be directly caused by local freshwater fluxes. Instead, it can be caused indirectly through winds via a reduced wind‐driven gyre circulation and salinity transport associated to this circulation, as seen in the higher‐resolution run. |
format |
Article in Journal/Newspaper |
author |
D. A. Putrasahan K. Lohmann J.‐S. vonStorch J. H. Jungclaus O. Gutjahr H. Haak |
author_facet |
D. A. Putrasahan K. Lohmann J.‐S. vonStorch J. H. Jungclaus O. Gutjahr H. Haak |
author_sort |
D. A. Putrasahan |
title |
Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
title_short |
Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
title_full |
Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
title_fullStr |
Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
title_full_unstemmed |
Surface Flux Drivers for the Slowdown of the Atlantic Meridional Overturning Circulation in a High‐Resolution Global Coupled Climate Model |
title_sort |
surface flux drivers for the slowdown of the atlantic meridional overturning circulation in a high‐resolution global coupled climate model |
publisher |
American Geophysical Union (AGU) |
publishDate |
2019 |
url |
https://doi.org/10.1029/2018MS001447 https://doaj.org/article/84cb4697dc2d4e0aa9e1b100733b867f |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 5, Pp 1349-1363 (2019) |
op_relation |
https://doi.org/10.1029/2018MS001447 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2018MS001447 https://doaj.org/article/84cb4697dc2d4e0aa9e1b100733b867f |
op_doi |
https://doi.org/10.1029/2018MS001447 |
container_title |
Journal of Advances in Modeling Earth Systems |
container_volume |
11 |
container_issue |
5 |
container_start_page |
1349 |
op_container_end_page |
1363 |
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1766131931270873088 |