On the basis of the simple dynamic model of circulation developed for the East China Sea in References [1] and [2], the present paper proposes a more complete
Having proved the stochastic model of air-sea interaction given by Mitchell (1956) to be a particular case of stochastic-dynamic model with linear air-sea feed
The principal variability patterns (EOF) of the anomalies of total heat transfer from ocean to atmosphere computed from 30 years’ monthly averaged data over t