Lake-Effect Snow Storms on Lake Michigan, USA
Lake-Effect Snow Storms on Lake Michigan, USA
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美国密歇根湖的湖泊效应暴风雪
DOI：
10.1007/978-94-009-7890-4_6
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发表时间：
1982
影响因子：
3.2
通讯作者：
R. D. Kelly
中科院分区：
文献类型：
--
作者：
R. Braham;R. D. Kelly
三种不同的对流模式，在湖效应的暴风雪在密歇根湖，美国：风平行带的云和降水由于水平滚动对流;深，岸平行云带与lakeinduced，中低压中心;和湖中部云带从湖岸的陆风会聚。
Examples are presented of three different convective patterns in lake-effect snow storms over Lake Michigan, USA: windparallel bands of clouds and precipitation due to horizontal-roll convection; deep, shore-parallel cloud bands associated with lakeinduced, meso low pressure centers; and midlake cloud bands resulting from the convergence of land breezes from the lake shores.