Sensitivity of Sea Surface Temperature Intraseasonal Oscillation to Diurnal Atmospheric Forcings in an OGCM
Abstract The diurnal cycle is a dominant mode of sea surface temperature (SST) variability in trop-ical oceans, that influences air-sea interaction and climate processes. Diurnal variability of SST generally ranges from ~0.1 to 2.0◦C and is controlled by atmospheric fluxes of heat and momentum. In t...
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| Language: | en_US |
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2018
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| Online Access: | http://etd.iisc.ernet.in/2005/3347 http://etd.iisc.ernet.in/abstracts/4212/G25741-Abs.pdf |