AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model
Abstract The Atlantic meridional overturning circulation (AMOC) is one of the most important characteristics of an ocean model run. Using the depth (z) and density frameworks, we analyze how the sinking and diapycnal transformations defining the AMOC as well as AMOC strength and variability react to...
Published in: | Journal of Advances in Modeling Earth Systems |
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ftdoajarticles:oai:doaj.org/article:74853bd663a04a8d9640b2611e4f18d8 2023-05-15T17:34:32+02:00 AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model Dmitry Sidorenko Sergey Danilov Vera Fofonova William Cabos Nikolay Koldunov Patrick Scholz Dmitry V. Sein Qiang Wang 2020-12-01T00:00:00Z https://doi.org/10.1029/2020MS002317 https://doaj.org/article/74853bd663a04a8d9640b2611e4f18d8 EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2020MS002317 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2020MS002317 https://doaj.org/article/74853bd663a04a8d9640b2611e4f18d8 Journal of Advances in Modeling Earth Systems, Vol 12, Iss 12, Pp n/a-n/a (2020) Physical geography GB3-5030 Oceanography GC1-1581 article 2020 ftdoajarticles https://doi.org/10.1029/2020MS002317 2022-12-31T15:32:18Z Abstract The Atlantic meridional overturning circulation (AMOC) is one of the most important characteristics of an ocean model run. Using the depth (z) and density frameworks, we analyze how the sinking and diapycnal transformations defining the AMOC as well as AMOC strength and variability react to mesh refinement from low to higher resolution in two model runs driven by the CORE‐II forcing. Both runs can represent the key locations of sinking and diapycnal transformations behind AMOC, that is, northeastern North Atlantic. Although their spatial patterns do not change significantly with resolution in both frameworks as the consequence of the same atmospheric forcing, the quantitative differences, reaching several sverdrups, are seen in different locations between two model runs for both frameworks. In particular, the refinement leads to the strongest differences in the vertical transport and diapycnal transformations in the latitude range between 30°N and 55°N. The z framework emphasizes the role of localized upwelling around the Gulf Stream separation site, whereas the density framework emphasizes the contribution of (spurious) diapycnal mixing around the Grand Banks. Both effects are reduced in the higher‐resolution run, leading to higher AMOC south of 26°N as compared to the low‐resolution run, despite the AMOC maxima, located at high latitudes, are higher in the low‐resolution run. We suggest that both AMOC frameworks should be used routinely in standard analyses, including forthcoming intercomparison projects. Article in Journal/Newspaper North Atlantic Sea ice Directory of Open Access Journals: DOAJ Articles Journal of Advances in Modeling Earth Systems 12 12 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Physical geography GB3-5030 Oceanography GC1-1581 |
spellingShingle |
Physical geography GB3-5030 Oceanography GC1-1581 Dmitry Sidorenko Sergey Danilov Vera Fofonova William Cabos Nikolay Koldunov Patrick Scholz Dmitry V. Sein Qiang Wang AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
topic_facet |
Physical geography GB3-5030 Oceanography GC1-1581 |
description |
Abstract The Atlantic meridional overturning circulation (AMOC) is one of the most important characteristics of an ocean model run. Using the depth (z) and density frameworks, we analyze how the sinking and diapycnal transformations defining the AMOC as well as AMOC strength and variability react to mesh refinement from low to higher resolution in two model runs driven by the CORE‐II forcing. Both runs can represent the key locations of sinking and diapycnal transformations behind AMOC, that is, northeastern North Atlantic. Although their spatial patterns do not change significantly with resolution in both frameworks as the consequence of the same atmospheric forcing, the quantitative differences, reaching several sverdrups, are seen in different locations between two model runs for both frameworks. In particular, the refinement leads to the strongest differences in the vertical transport and diapycnal transformations in the latitude range between 30°N and 55°N. The z framework emphasizes the role of localized upwelling around the Gulf Stream separation site, whereas the density framework emphasizes the contribution of (spurious) diapycnal mixing around the Grand Banks. Both effects are reduced in the higher‐resolution run, leading to higher AMOC south of 26°N as compared to the low‐resolution run, despite the AMOC maxima, located at high latitudes, are higher in the low‐resolution run. We suggest that both AMOC frameworks should be used routinely in standard analyses, including forthcoming intercomparison projects. |
format |
Article in Journal/Newspaper |
author |
Dmitry Sidorenko Sergey Danilov Vera Fofonova William Cabos Nikolay Koldunov Patrick Scholz Dmitry V. Sein Qiang Wang |
author_facet |
Dmitry Sidorenko Sergey Danilov Vera Fofonova William Cabos Nikolay Koldunov Patrick Scholz Dmitry V. Sein Qiang Wang |
author_sort |
Dmitry Sidorenko |
title |
AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
title_short |
AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
title_full |
AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
title_fullStr |
AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
title_full_unstemmed |
AMOC, Water Mass Transformations, and Their Responses to Changing Resolution in the Finite‐VolumE Sea Ice‐Ocean Model |
title_sort |
amoc, water mass transformations, and their responses to changing resolution in the finite‐volume sea ice‐ocean model |
publisher |
American Geophysical Union (AGU) |
publishDate |
2020 |
url |
https://doi.org/10.1029/2020MS002317 https://doaj.org/article/74853bd663a04a8d9640b2611e4f18d8 |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_source |
Journal of Advances in Modeling Earth Systems, Vol 12, Iss 12, Pp n/a-n/a (2020) |
op_relation |
https://doi.org/10.1029/2020MS002317 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2020MS002317 https://doaj.org/article/74853bd663a04a8d9640b2611e4f18d8 |
op_doi |
https://doi.org/10.1029/2020MS002317 |
container_title |
Journal of Advances in Modeling Earth Systems |
container_volume |
12 |
container_issue |
12 |
_version_ |
1766133406111891456 |