The Structure and Formation Mechanism of Transversal Cloud Bands Associated with the Japan-Sea Polar-Airmass Convergence Zone-Reference-Cited by-同舟云学术

The Structure and Formation Mechanism of Transversal Cloud Bands Associated with the Japan-Sea Polar-Airmass Convergence Zone

Published:2010 Issue:4 Volume:88 Page:625-648
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:

EITO Hisaki¹,MURAKAMI Masataka¹,MUROI Chiashi²,KATO Teruyuki¹,HAYASHI Syugo¹,KUROIWA Hiroshi³,YOSHIZAKI Masanori⁴

Affiliation:

1. Meteorological Research Institute, Japan Meteorological Agency

2. Numerical Prediction Division, Forecast Department, Japan Meteorological Agency

3. Support Center for Advanced Telecommunications Technology Research, Foundation

4. Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Link

http://www.jstage.jst.go.jp/article/jmsj/88/4/88_4_625/_pdf

Reference43 articles.

1. 1) Arakawa, S., and Research Group on Mesoscale Meteorology of Marine Development, JMA, 1988: On the mesoscale structure of the cloud band system over Japan Sea in winter monsoon period.—A mesoscale observation on board R/V Keifu-Maru. Tenki, 35, 237-248 (in Japanese).

2. 2) Asai, T., 1970a: Three-dimensional features of thermal convection in a plane Couette flow. J. Meteor. Soc. Japan, 48, 18-29.

3. 3) Asai, T., 1970b: Stability of a plane parallel flow with variable vertical shear and unstable stratification. J. Meteor. Soc. Japan, 48, 129-139.

4. 4) Asai, T., 1972: Thermal instability of a shear flow turning the direction with height. J. Meteor. Soc. Japan, 50, 525-532.

5. A Numerical Experiment of Airmass Transformation Processes over Warmer Sea

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