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Fig. 2
Buoyancy frequency N(z) for an example with 3 steps. Convective layers of size d, within whichN(z) = 0, are separated by stably stratified interfaces of size l, within whichN(z) > 0, given by Eq. (31). The amplitude of the peaks, N0, is calculated so that the mean stratification equals 
. Here, 
.
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