X-Band Dual-Polarization Radar Observations of Precipitation Core Development and Structure in a Multi-Cellular Storm over Zoshigaya, Japan, on August 5, 2008
Author:
Affiliation:
1. National Research Institute for Earth Science and Disaster Prevention
2. Department of Environmental Atmospheric Sciences, Pukyong National University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj/90/5/90_2012-509/_pdf
Reference42 articles.
1. 1) Battan, L. J., 1953: Duration of convective radar cloud unit. Bull. Amer. Meteor. Soc., 34, 227-228.
2. 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., 41, 1711-1732.
3. An Examination of Propagation Effects in Rainfall on Radar Measurements at Microwave Frequencies
4. 4) Bringi, V. N., and V. Chandrasekar, 2001: Polarimetric Doppler Weather Radar: Principles and Applications. Cambridge University Press, 648 pp.
5. 6) Carey, L. D., S. A. Rutledge, D. A. Ahijevych, and T. D. Keenan, 2000: Correction propagation effects in C-band polarimetric radar observations of tropical convection using differential propagation phase. J. Appl. Meteor., 39, 1405-1433.
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