The Response of the Surface Wind Speed to the Synoptic Pressure Gradient in Central Japan
Author:
Affiliation:
1. Institute of Geoscience, University of Tsukuba
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/69/3/69_3_389/_pdf
Reference13 articles.
1. Anzai, M., 1973: The automated meteorological data acquisition system. Tenki, 20, 335-344 (in Japanese).
2. Brenner, I.S., 1980: Arizona cool season surface wind and pressure gradient study. Bull. Amer. Meteor. Soc., 61, 114-120.
3. Danard, M., 1988: A diagnostic method for computing the surface wind from the geostrophic wind including the effects of baroclinity. Mon. Wea. Rev., 116, 2712-2716.
4. Fujibe, F., 1985: An effect of pressure gradient on the diurnal variation of wind in the atmospheric boundary layer. J. Meteor. Soc. Japan, 63, 52-59.
5. Hasse, L. and Wagner, V., 1971: On the relationship between geostrophic and surface wind at sea. Mon. Wea. Rev., 99, 255-260.
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