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Hae-Kyung Lee Drbohlav, Silvio Gualdi, and Antonio Navarra

the fact that the surge of cold water, induced by the upwelling, does not always penetrate into the mixed layer and affect the mixed layer temperature [see Eq. (2a) ]. Since, the entrainment velocity in (2a) is the relative velocity with respect to the mixed layer bottom, which also changes in time (∂ h ′ ML /∂ t ), the effect of the entrainment and detrainment in the linear approximation seems often smaller than that of the upwelling and downwelling. c. Characteristics of the IODM in El Niño

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