A Study of Fukui Heavy Rainfall in 2004
Author:
Affiliation:
1. Frontier Research Center 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/86/2/86_2_369/_pdf
Reference8 articles.
1. Structure of the Band-Shaped Precipitation System Inducing the Heavy Rainfall Observed over Northern Kyushu, Japan on 29 June 1999
2. Formation Factors of 2004 Niigata-Fukushima and Fukui Heavy Rainfalls and Problems in the Predictions using a Cloud-Resolving Model
3. Formation and Maintenance Processes of a Stationary Band-shaped Heavy Rainfall Observed in Niigata on 4 August 1998.
4. Reason for the Failure of the Simulation of Heavy Rainfall during X-BAIU-01-Importance of a Vertical Profile of Water Vapor for Numerical Simulations-
5. Ninomiya, K., T. Akiyama, S. Yoshizumi, K. Yamazaki, and H. Sakakibara, 1980: Heavy rainfall in the Baiu frontal zone. Meteor. Res. Notes, 138, 277 pp (in Japanese).
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1. Toward an Understanding of the Madden-Julian Oscillation: With a Mesoscale-Convection-Resolving Model of 0.2 Degree Grid;Advances in Meteorology;2011
2. Development of a Nonhydrostatic Version of the Mesoscale-Convection-Resolving Model and its Application to the Eyewall and Spiral Rainbands of Tropical Cyclones;Journal of the Meteorological Society of Japan. Ser. II;2010
3. Relationship between High-Impact Weather Events in Japan and Propagation of Rossby Waves along the Asian Jet in July 2004;Journal of the Meteorological Society of Japan. Ser. II;2009
4. A Study of the Mesoscale Convective System under Vertical Shear Flow in the Latently Unstable Atmosphere with North-South Asymmetry;Journal of the Meteorological Society of Japan. Ser. II;2009
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