| Registro completo |
| Provedor de dados: |
ArchiMer
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| País: |
France
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| Título: |
Atlantic Meridional Overturning Circulation: Observed Transport and Variability
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| Autores: |
Frajka-williams, Eleanor
Ansorge, Isabelle J.
Baehr, Johanna
Bryden, Harry L.
Chidichimo, Maria Paz
Cunningham, Stuart A.
Danabasoglu, Gokhan
Dong, Shenfu
Donohue, Kathleen A.
Elipot, Shane
Heimbach, Patrick
Holliday, N. Penny
Hummels, Rebecca
Jackson, Laura C.
Karstensen, Johannes
Lankhorst, Matthias
Le Bras, Isabela A.
Lozier, M. Susan
Mcdonagh, Elaine L.
Meinen, Christopher S.
Mercier, Herle
Moat, Bengamin I.
Perez, Renellys C
Piecuch, Christopher G.
Rhein, Monika
Srokosz, Meric A.
Trenberth, Kevin E.
Bacon, Sheldon
Forget, Gael
Goni, Gustavo
Kieke, Dagmar
Koelling, Jannes
Lamont, Tarron
Mccarthy, Gerard D.
Mertens, Christian
Send, Uwe
Smeed, David A.
Speich, Sabrina
Van Den Berg, Marcel
Volkov, Denis
Wilson, Chris
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| Data: |
2019-06
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| Ano: |
2019
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| Palavras-chave: |
Meridional overturning circulation
Thermohaline circulation
Observing systems
Ocean heat transport
Carbon storage
Moorings
Circulation variability
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| Resumo: |
The Atlantic Meridional Overturning Circulation (AMOC) extends from the Southern Ocean to the northern North Atlantic, transporting heat northwards throughout the South and North Atlantic, and sinking carbon and nutrients into the deep ocean. Climate models indicate that changes to the AMOC both herald and drive climate shifts. Intensive trans-basin AMOC observational systems have been put in place to continuously monitor meridional volume transport variability, and in some cases, heat, freshwater and carbon transport. These observational programs have been used to diagnose the magnitude and origins of transport variability, and to investigate impacts of variability on essential climate variables such as sea surface temperature, ocean heat content and coastal sea level. AMOC observing approaches vary between the different systems, ranging from trans-basin arrays (OSNAP, RAPID 26°N, 11°S, SAMBA 34.5°S) to arrays concentrating on western boundaries (e.g., RAPID WAVE, MOVE 16°N). In this paper, we outline the different approaches (aims, strengths and limitations) and summarize the key results to date. We also discuss alternate approaches for capturing AMOC variability including direct estimates (e.g., using sea level, bottom pressure, and hydrography from autonomous profiling floats), indirect estimates applying budgetary approaches, state estimates or ocean reanalyses, and proxies. Based on the existing observations and their results, and the potential of new observational and formal synthesis approaches, we make suggestions as to how to evaluate a comprehensive, future-proof observational network of the AMOC to deepen our understanding of the AMOC and its role in global climate.
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| Tipo: |
Text
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| Idioma: |
Inglês
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| Identificador: |
https://archimer.ifremer.fr/doc/00503/61507/65342.pdf
https://archimer.ifremer.fr/doc/00503/61507/65343.pdf
DOI:10.3389/fmars.2019.00260
https://archimer.ifremer.fr/doc/00503/61507/
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| Editor: |
Frontiers Media SA
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| Relação: |
info:eu-repo/grantAgreement/EC/H2020/727852/EU//Blue-Action
info:eu-repo/grantAgreement/EC/FP7/633211/EU//AtlantOS
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| Formato: |
application/pdf
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| Fonte: |
Frontiers In Marine Science (2296-7745) (Frontiers Media SA), 2019-06 , Vol. 6 , N. 260 , P. 18p.
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| Direitos: |
info:eu-repo/semantics/openAccess
restricted use
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