Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes

Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes

Abstract A multimodel, multiresolution ensemble using Coupled Model Intercomparison Project Phase 6 (CMIP6) High Resolution Model Intercomparison Project (HighResMIP) coupled experiments is used to assess the performance of key aspects of the North Atlantic circulation. The Atlantic Meridional Overt...

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Detalles Bibliográficos
Autores principales: Malcolm J. Roberts, Laura C. Jackson, Christopher D. Roberts, Virna Meccia, David Docquier, Torben Koenigk, Pablo Ortega, Eduardo Moreno‐Chamarro, Alessio Bellucci, Andrew Coward, Sybren Drijfhout, Eleftheria Exarchou, Oliver Gutjahr, Helene Hewitt, Doroteaciro Iovino, Katja Lohmann, Dian Putrasahan, Reinhard Schiemann, Jon Seddon, Laurent Terray, Xiaobiao Xu, Qiuying Zhang, Ping Chang, Stephen G. Yeager, Frederic S. Castruccio, Shaoqing Zhang, Lixin Wu
Formato: article
Lenguaje:EN
Publicado: American Geophysical Union (AGU) 2020
Materias:
ocean circulation
Atlantic
model resolution
AMOC
future projection
Physical geography
GB3-5030
Oceanography
GC1-1581
Acceso en línea:https://doaj.org/article/8b74ce5a5c8441f78474dc0b3e65bb46
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Sumario:Abstract A multimodel, multiresolution ensemble using Coupled Model Intercomparison Project Phase 6 (CMIP6) High Resolution Model Intercomparison Project (HighResMIP) coupled experiments is used to assess the performance of key aspects of the North Atlantic circulation. The Atlantic Meridional Overturning Circulation (AMOC), and related heat transport, tends to become stronger as ocean model resolution is enhanced, better agreeing with observations at 26.5°N. However, for most models the circulation remains too shallow compared to observations and has a smaller temperature contrast between the northward and southward limbs of the AMOC. These biases cause the northward heat transport to be systematically too low for a given overturning strength. The higher‐resolution models also tend to have too much deep mixing in the subpolar gyre. In the period 2015–2050 the overturning circulation tends to decline more rapidly in the higher‐resolution models, which is related to both the mean state and to the subpolar gyre contribution to deep water formation. The main part of the decline comes from the Florida Current component of the circulation. Such large declines in AMOC are not seen in the models with resolutions more typically used for climate studies, suggesting an enhanced risk for Northern Hemisphere climate change. However, only a small number of different ocean models are included in the study.

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