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• W2072829963 abstract "Abstract An atmospheric general circulation model (AGCM), a simplified atmospheric model (SAM) of surface heat flux, and various idealized analytic models have been used to investigate the atmospheric response over the North Atlantic to SST anomalies including a general cooling associated with a weakened thermohaline circulation. Latent heating dominates the surface heat flux response, while sensible heating plays an important secondary role. The total heat flux response is weaker than presumed in recent studies using ocean models under highly idealized surface boundary conditions. This implies that stability of the thermohaline circulation to high-latitude freshening in more sophisticated coupled systems (that incorporate either AGCMs or models like SAM) will be increased. All three kinds of atmospheric models exhibit nonrestorative behavior away from the anomaly peak that is primarily associated with the advection of cooled air eastward. This simple picture is complicated in the AGCM by the fact that th..." @default.
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• W2072829963 date "1995-09-01" @default.
• W2072829963 modified "2023-09-25" @default.
• W2072829963 title "Modeling the Surface Heat Flux Response to Long-Lived SST Anomalies in the North Atlantic" @default.
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• W2072829963 doi "https://doi.org/10.1175/1520-0442(1995)008<2161:mtshfr>2.0.co;2" @default.
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