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- W2480856849 abstract "Variability associated with the Asian-Australian monsoon system has been recognized in recent years as resulting from air-sea coupled processes. This points to the importance of ocean dynamics that controls the time-varying sea surface temperature (SST) signals. Aside from the surface heat flux forcing, many oceanic processes can produce changes in SST in the Asian-Australian monsoon regions: lateral advection by oceanic mean/eddy flows, enhanced tidal mixing in shallow seas, variability in the thermocline depth induced either locally or remotely (via wave-guides) in the Pacific and Indian Oceans, wind-induced coastal upwelling, and salinity stratification related to the monsoonal rainfall and river runoff. This article reviews some of these oceanic processes on the basis of our understanding achieved in recent years." @default.
- W2480856849 created "2016-08-23" @default.
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- W2480856849 date "2011-04-01" @default.
- W2480856849 modified "2023-09-27" @default.
- W2480856849 title "OCEANIC PROCESSES INFLUENCING SST IN REGIONS RELATED TO THE ASIAN-AUSTRALIAN MONSOON SYSTEM" @default.
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- W2480856849 doi "https://doi.org/10.1142/9789814343411_0030" @default.
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