Arid
报告编号PB2008111013
Frontogenesis, Conditional Symmetric Instability and Microphysics: A Rare Desert Snow Event.
Orow, H; Czyzyk, S.
英文摘要During the overnight and early morning hours of November 21, 2004, a strong low pressure system brought up to 12 inches of snowfall to the deserts of San Bernardino County in Southern California. Snow accumulations of this magnitude over the deserts of Southern California are rare. The study of this event concentrates on the town of Yucca Valley, CA which received between 8 and 12 inches of snowfall. Yucca Valley is located in the south central portion of San Bernardino County at an elevation of 3500 ft (Fig. 1). This paper will examine the ingredients that came together to produce this heavy snowfall event, particularly how strong dynamics and favorable cloud microphysics can overcome the lack of a deep layer moisture tap to produce significant snowfall accumulations. This case also underscored the importance of utilizing analysis skills and maintaining a high level of situational awareness in order to deduce the presence of mesoscale processes that may require adjustments to model predictions.
英文关键词Frontogenesis Deserts Snowfall Microphysics Southern California Cloud physics Meso scale phenomena Yucca Valley(California)
出版年2008
语种英语
国家United States
URLhttp://r.cnki.net/KCMS/detail/detail.aspx?DbCode=KJBG&dbname=KJBGW&filename=59fb2f4731c97d1d54a021da
来源机构National Oceanic and Atmospheric Administration
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/273576
推荐引用方式
GB/T 7714
Orow, H,Czyzyk, S.. Frontogenesis, Conditional Symmetric Instability and Microphysics: A Rare Desert Snow Event.,2008.
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