Abstract
An inviscid model for the sea breeze derived from the viscous model of Li and Smith (J Atmos Sci 67:2752–2765, 2010) [thereafter used by Jiang (J Atmos Sci 69:1890–1909, 2012)] has been considered. The apparent singularities appearing in the inviscid case has been analyzed rigorously and shown that they can be removed easily by taking limits of the Fourier transform of the solutions. It is also shown that the inviscid solutions have earlier onset of onshore winds in comparison to the viscous solutions.
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Schedule a callMore From: International journal of advances in engineering sciences and applied mathematics
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