Characteristics of Summertime Afternoon Rainfall and Its Environmental Conditions in and around the Nobi Plain

Author:

Takemi Tetsuya1

Affiliation:

1. Disaster Prevention Research Institute, Kyoto University

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Reference14 articles.

1. Bluestein, H. B., 1993: Synoptic-Dynamic Meteorology in Midlatitudes, Vol. II, Oxford Univ. Press, 594 pp.

2. Kawano, K., Y. Hirokawa, and H. Ohno, 2004: Diagnosis of air-mass thunderstorm days using radiosonde data: The summer Kanto area under the Pacific subtropical anticyclone. Tenki, 51, 17-30.

3. Kobayashi, F., T. Takano, and T. Takamura, 2011: Isolated cumulonimbus initiation observed by 95-GHz FM-CW radar, X-band radar, and photogrammetry in the Kanto region, Japan. SOLA, 7, 125-128.

4. Kuwagata, T., 1997: An analysis of summer rain showers over central Japan and its relation with the thermally induced circulation. J. Meteor. Soc. Japan, 75, 513-527.

5. Nagata, K., 2011: Quantitative precipitation estimation and quantitative precipitation forecasting by the Japan Meteorological Agency. RSMC Tokyo-Typhoon Center Technical Review, 13, 37-50. Available online at: http://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/techrev/text13-2.pdf.

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