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contributor authorKelly, Robert D.
date accessioned2017-06-09T14:23:14Z
date available2017-06-09T14:23:14Z
date copyright1982/07/01
date issued1982
identifier issn0022-4928
identifier otherams-18389.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154388
description abstractThe boundary-layer structure and circulation over Lake Michigan were probed with a Doppler radar and an aircraft during a lake-effect snow storm on 9 December 1978. Evidence is presented that observed wind-parallel echo bands and satellite cloud bands resulted from horizontal-roll convection in the boundary layer. The organization of precipitation within the roll field is discussed, and the roll geometry is compared with cases of dry horizontal-roll convection reported in the literature.
publisherAmerican Meteorological Society
titleA Single Doppler Radar Study of Horizontal-Roll Convection in a Lake-Effect Snow Storm
typeJournal Paper
journal volume39
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1982)039<1521:ASDRSO>2.0.CO;2
journal fristpage1521
journal lastpage1531
treeJournal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 007
contenttypeFulltext


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