Dual Doppler Radar Analysis of an Intense Mesoscale Rainband Generated along the Baiu Front in 1988
Author:
Affiliation:
1. Observations Department, Japan Meteorological Agency (JMA)
2. Institute for Hydrospheric-Atmospheric Sciences, Nagoya University
3. Forecast Department, JMA
4. Meteorological Research Institute, JMA
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/73/2/73_2_139/_pdf
Reference42 articles.
1. Akiyama, T., 1973: The large-scale aspects of the characteristic features of the Baiu front with special emphasis on the relation among the ageostrophic low-level jet stream, moist tongue, convective warming, convergence zone within the Baiu front and heavy rainfall. Papers Meteor. Geoph., 24, 157-186.
2. Akiyama, T., 1974: Mesoscale organization of cumulus convection in the large-scale rainband in the Baiu season. J. Meteor. Soc. Japan, 52, 448-451.
3. Akiyama, T., 1978: Variation of thermal stratification in subtropical medium-scale disturbances. J. Meteor. Soc. Japan, 57, 587-598.
4. Akiyama, T., 1979: Thermal stratification in Baiu frontal medium-scale disturbances with heavy rainfalls. J. Meteor. Soc. Japan, 57, 587-598.
5. Akiyama, T., 1984a: A medium-scale cloud cluster in a Baiu front. Part 1: Evolution process and fine structure. J. Meteor. Soc. Japan, 62, 485-504.
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