Fig. 9b. Nonlinear WN-1 streamfunction (ψ) with no linear forcing, after 240h for a barotropic nondivergent vortex in a resting environment on a β-plane. These "anti-β gyres" result from nonlinear interaction between WN-1 and WN-2
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Fig. 9b. Nonlinear WN-1 streamfunction (ψ) with no linear forcing, after 240h for a barotropic nondivergent vortex in a resting environment on a β-plane. These "anti-β gyres" result from nonlinear interaction between WN-1 and WN-2 |