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Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean

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Figure

Fig. 1. Three-layer model ocean.
Fig. 2. Vertical density profiles in the Gotland Basin, Baltic Sea, 26.–28.08.1986: (a) 57 ◦ 31,6 0 N, 20 ◦ 34,2 0 E; (b) 57 ◦ 37,0 0 N, 20 ◦ 32,4 0 E; (c) 57 ◦ 38,5 0 N, 20 ◦ 36,1 0 E; (d) 57 ◦ 38,0 0 N, 20 ◦ 42,5 0 E.
Table 1. Conditions of vanishing of the coupling coefficients. Symbol “+” means that the corresponding coefficient never vanishes and “0”

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