A Dual-Doppler Radar Study of Longitudinal-Mode Snowbands
Author:
Affiliation:
1. Division of Science Education, Osaka Kyoiku University
2. Institute of Low Temperature Science, Hokkaido University
3. Institute for Hydrospheric-Atmospheric Sciences, Nagoya University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/78/4/78_4_381/_pdf
Reference13 articles.
1. Asai, T., 1970: Three-dimensional features of thermal convection in a plane Couette flow. J. Meteor. Soc. Japan, 48, 18-29.
2. Asuma, Y. and K. Kikuchi, 1987: Snowfall properties in the Sapporo city area and the occurrence frequency of radar echoes over the Ishikari Bay, Hokkaido, Japan. Geophys. Bull. Hokkaido Univ., 49, 317-330 (in Japanese with English abstract).
3. Brown, R. A., 1970: A secondary flow model for the planetary boundary layer. J. Atmos. Sci., 27, 742-757.
4. Fujiyoshi, Y., K. Tsuboki, S. Satoh and G. Wakahama, 1992: Three-dimensional radar echo structure of a snow band formed on the lee side of a mountain. J. Meteor. Soc. Japan, 70, 11-24.
5. Fujiyoshi, Y., N. Yoshimoto and T. Takeda, 1998: A dual-Doppler radar study of longitudinal-mode snow-bands. Part I: A three-dimensional kinematic structure of meso-γ-scale convective cloud systems within a longitudinal-mode snowband. Mon. Wea. Rev., 126, 72-91.
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