Abstract:SummaryAn attempt is made to study certain characteristic features of the "dynamic initialization" (DI) technique, incorporating the averaging scheme. The limited area barotropic version of the primitive equation model is used. Numerical experiments are performed by varying the number of time-steps during the iterations, N, from 3 to 7. It is found that forN = 5, the least ageostrophic wind component (Area-mean value) is obtained. However, the least "noise" is generated during the time-integration, for N = 6, … Show more
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