Abstract
In order to avoid the truncation errors near the typhoon center, which arise in the course of numerical computation, and to obtain the stream function in the vicinity of typhoon precisely, the balance equation is separated into two parts; the one is corresponding to the circular symmetric field and the other, to the residual field. The stream function corresponding to the circular symmetric field is easily obtained by the gradient wind equation. After the condition for existence of solutions of the balance equation corresponding to the residual field is examined, the point relaxation procedure to solve this equation is proposed. An example of this solving method, applying to the typhoon Harriet, is presented also.
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