Formation Mechanism of a Stationary Line-Shaped Precipitation System in the Kinki District, Japan —Case Study on 1 September 2015 Event—
Author:
Affiliation:
1. Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, Japan
2. Earth Observation Research and application Center, Japan Aerospace Exploration Agency, Tsukuba, Japan
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj/99/2/99_2021-017/_pdf
Reference23 articles.
1. Banacos, P. C., and D. M. Schultz,, 2005: The use of moisture flux convergence in forecasting convective initiation: Historical and operational perspectives. Wea. Forecasting, 20, 351-366.
2. Bluestein, H. B., and M. H. Jain, 1985: Formation of mesoscale lines of precipitation: Severe squall lines in Oklahoma during the spring. J. Atmos. Sci., 42, 1711-1732.
3. Gallus, W. A., Jr., N. A. Snook, and E. V. Johnson, 2008: Spring and summer severe weather reports over the Midwest as a function of convective mode: A preliminary study. Wea. Forecasting, 23, 101-113.
4. Higashi, K., Y. Kiyohara, M. D. Yamanaka, Y. Shibagaki, M. Kusuda, and T. Fujii, 2010: Multiscale features of line-shaped precipitation system generation in central Japan during late baiu season. J. Meteor. Soc. Japan, 88, 909-930.
5. Houze, R. A., Jr., 1993: Cloud Dynamics. International Geophysics Series, No. 53, Academic Press, 573 pp.
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