Characteristics of Low-level Jets in Shanghai during the 2008-2009 Warm Seasons as Inferred from Wind Profiler Radar Data
Author:
Affiliation:
1. Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University
2. Shanghai Meteorological Bureau
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj/90/6/90_2012-603/_pdf
Reference45 articles.
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2. 2) Bell, T. L., and N. Reid, 1993: Detecting the diurnal cycle of rainfall using satellite observations. J. Appl. Meteor., 32, 311-322.
3. 3) Blackadar, A. K., 1957: Boundary layer wind maxima and their significance for the growth of nocturnal inversions. Bull. Amer. Meteor. Soc, 38, 283-290.
4. 4) Bonner, W. D., 1968: Climatology of the low level jet. Mon. Wea. Rev, 96, 833-850.
5. 5) Burk, S. D., and W. T. Thompson, 1996: The summertime low-level jet and marine boundary layer structure along the California coast. Mon. Wea. Rev, 124, 668-686.
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