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contributor authorSalmon, Ellen M.
contributor authorSmith, Phillip J.
date accessioned2017-06-09T14:39:52Z
date available2017-06-09T14:39:52Z
date copyright1980/05/01
date issued1980
identifier issn0003-0007
identifier otherams-23946.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160563
description abstractBased on detailed surface analyses and National Meteorological Center (NMC) facsimile products, the evolution of the January 1978 midwestern blizzard-producing cyclone is described. The behavior of the storm is contrasted with the actions of typical winter cyclones. Forecasts by the Limited-Area Fine Mesh (LFM) numerical model are compared with observed conditions. An injection of polar air, resulting in the revitalization of the baroclinic zone, and concurrent strong upper-air flow are found to be important factors in the dramatic intensification of the low. The movement and deepening of the low, although not unprecedented, were found to deviate substantially from normal winter cyclone behavior. Although LFM forecasts underestimated the deepening of the low, the amount of predicted intensification was substantial.
publisherAmerican Meteorological Society
titleFocus on Forecasting: A Synoptic Analysis of the 25–26 January 1978 Blizzard Cyclone in the Central United States
typeJournal Paper
journal volume61
journal issue5
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/1520-0477(1980)061<0453:FOFASA>2.0.CO;2
journal fristpage453
journal lastpage453
treeBulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 005
contenttypeFulltext


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