On Gradient Winds

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چکیده

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Computation and Uses of Gradient Winds

The viewpoint is taken that in large port>ions of the atmospherc, wind spcclds (V,,), divergence (D,?), and vor-ticity (r,?) obtained under the gradient wind assnmptiorl are considerably morc accurate representations of true conditions than those one obtains from the geostrophic assumption. Equations are derived for computing V,,, D,,, and rgl. The equation for the vorticity of gradicnt' winds ...

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ژورنال

عنوان ژورنال: Journal of the Meteorological Society of Japan. Ser. II

سال: 1936

ISSN: 0026-1165,2186-9057

DOI: 10.2151/jmsj1923.14.4_153