Three-Dimensional Radar Echo Structure of a Snow Band Formed on the Lee Side of a Mountain-Reference-Cited by-同舟云学术

Three-Dimensional Radar Echo Structure of a Snow Band Formed on the Lee Side of a Mountain

Published:1992 Issue:1 Volume:70 Page:11-24
ISSN:0026-1165
Container-title:Journal of the Meteorological Society of Japan. Ser. II
language:en
Short-container-title:Journal of the Meteorological Society of Japan

Author:

Fujiyoshi Yasushi¹,Tsuboki Kazuhisa¹,Satoh Shinsuke¹,Wakahama Gorow¹

Affiliation:

1. Institute of Low Temperature Science, Hokkaido Univ

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Link

https://www.jstage.jst.go.jp/article/jmsj1965/70/1/70_1_11/_pdf

Reference22 articles.

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2. Asai, T., 1970: Stability of a plane parallel flow withvariable vertical shear and unstable stratification. J.Meteor. Soc. Japan, 48. 129-139.

3. Asuma, Y. and K. Kikuchi, 1987: Snowfall properties inthe Sapporo city area and the occurrence frequencyof radar echoes over the Ishikari Bay, Hokkaido,Japan (Japanese with English summary). Geophys.Bull. Hokkaido Univ., 49, 317-330.

4. Brown, R.A., 1970: A secondary flow model for the planetary boundary layer. J. Atrnos. Sci., 27, 742-757.

5. Brown, R.A.,1972: On the inflection point instability ofa stratified Ekman boundary layer. J. Atmos. Sci.,29, 850-859.

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