( 5 ) based on the complete form of vertical vorticity tendency equation , the effect of spatially non - uniform heating on the formation and variation of subtropical high is discussed
2.
The two analytic examples show that : if the heating and moistening due to convection at the switch - on point is much smaller than all the other terms in the tendency equation , then keeping the " on - off " switches the same as the basic state will produce the right tangent linear model and adjoint model
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