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    Focus on Forecasting: A Synoptic Analysis of the 25–26 January 1978 Blizzard Cyclone in the Central United States

    Source: Bulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 005::page 453
    Author:
    Salmon, Ellen M.
    ,
    Smith, Phillip J.
    DOI: 10.1175/1520-0477(1980)061<0453:FOFASA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Based 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.
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      Focus on Forecasting: A Synoptic Analysis of the 25–26 January 1978 Blizzard Cyclone in the Central United States

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4160563
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    • Bulletin of the American Meteorological Society

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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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    DSpace software copyright © 2002-2015  DuraSpace
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