Occurrence tendency of heavy rainfall or snowfall in the inland district of Japan in winter

Author:

ANDO Naoki1,UENO Kenichi2

Affiliation:

1. Mito Local Meteorological Office

2. Faculty of Life and Environmental Sciences, University of Tsukuba

Publisher

Japanese Society of Snow and Ice

Subject

General Medicine

Reference28 articles.

1. 安藤敏幸・岡田哲也・須田勝治・田口静・古山享嗣,2013:南岸低気圧による木曽山脈南部周辺の降雪特性.天気,60,15-20.

2. Araki, K. andM.Murakami, 2015:Numerical simulation of heavy snowfall and the potential role of ice nuclei in cloud formation and precipitation development. CAS/JSC WGNE Research Activities in Atmospheric and Oceanic Modelling, 45, 4.03-4.04.

3. Browning, K.A. and F. Hill, 1985:Mesoscale analysis of a polar trough intersecting with a polar front. Quart. J. Roy. Meteor. Soc., 111, 445-462.

4. Carlson, T.N., 1991: Mid-latitude Weather Systems. Routledge, NY, 507 pp.

5. Ebita, A., S. Kobayashi, Y. Ota,M.Moriya, R. Kumabe, K. Onogi, Y. Harada, S. Yasui, K. Miyaoka, K. Takahashi, H. Kamahori, C. Kobayashi, H. Endo, M. Soma, Y. Oikawa and T. Ishimizu, 2011:The Japanese 55-year reanalysis “JRA-55”:an interim report, SOLA, 7, 149-152.

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