Attribution of the seasonality of atmospheric heating changes over the western tropical Pacific with a focus on the spring season
Atmospheric diabatic heating, a major driving force of atmospheric circulation over the tropics, is strongly confined to the tropical western North Pacific (TWNP) region, with the global warmest sea surface temperature (SST). The changes in diabatic heating over the TWNP, which exert great impacts o...
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Veröffentlicht in: | Climate dynamics 2022-05, Vol.58 (9-10), p.2575-2592 |
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Sprache: | eng |
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