Relationship between the Upper-level Winds and the Horizontal Movement of Localized Heavy Rainfall in the Afternoon of Summer Days around Tokyo
Author:
Affiliation:
1. Institute for Space-Earth Environmental Research, Nagoya University
2. Tokyo Gakugei University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/sola/18/0/18_2022-002/_pdf
Reference18 articles.
1. Bunkers, M. J., B. A. Klimowski, J. W. Zeitler, R. L. Thompson, and M. L. Weisman, 2000: Predicting supercell motion using a new hodograph technique. Wea. Forecasting, 15, 61-79, doi:10.1175/1520-0434(2000)015<0061:PSMUAN>2.0.CO;2.
2. Bunkers, M. J., 2018: Observations of right-moving supercell motion forecast errors. Wea. Forecasting, 33, 145-159, doi:10.1175/WAF-D-17-0133.1.
3. Fujibe, F., 1988: Diurnal variations of precipitation and thunderstorm frequency in Japan in the warm season. Pap. Meteor. Geophys., 39, 79-94, doi:10.2467/mripapers.39.79.
4. Fujibe, F., K. Sakagami, K. Chubachi, and K. Yamashita, 2002: Surface wind patterns preceding short-time heavy rainfall in Tokyo in the afternoon of midsummer days. Tenki, 49, 395-405 (in Japanese with English abstract).
5. Fujibe, F., 2003: Long-term surface wind changes in the Tokyo metropolitan area in the afternoon of sunny days in the warm season. J. Meteor. Soc. Japan, 81, 141-149, doi:10.2151/jmsj.81.141.
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