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...

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Published in:Journal of Advances in Modeling Earth Systems
Main Authors: Dmitry Sidorenko, Sergey Danilov, Vera Fofonova, William Cabos, Nikolay Koldunov, Patrick Scholz, Dmitry V. Sein, Qiang Wang
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2020
Subjects:
Online Access:https://doi.org/10.1029/2020MS002317
https://doaj.org/article/74853bd663a04a8d9640b2611e4f18d8
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spelling 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
institution 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
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