Abstract
The present method is based on a decomposition of the velocity potential into two new functions. These two functions, forming a new system, can be stably integrated in opposite radial directions. A far-field boundary condition in free air is established at a finite radius by means of the asymptotic Guderley far-field expansion. Porous wind tunnel walls also can be handled by this method. A pronounced feature of this iterative method, considering only one new function at a time, is a rather high rate of convergence. The agreement with experimental data and other comparable methods is found to be very good.
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