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    A Collaborative Approach to Study Northwest Flow Snow in The Southern Appalachians

    Source: Bulletin of the American Meteorological Society:;2009:;volume( 090 ):;issue: 007::page 979
    Author:
    Keighton, Steve
    ,
    Lee, Laurence
    ,
    Holloway, Blair
    ,
    Hotz, David
    ,
    Zubrick, Steven
    ,
    Hovis, Jeffrey
    ,
    Votaw, Gary
    ,
    Perry, L. Baker
    ,
    Lackmann, Gary
    ,
    Yuter, Sandra E.
    ,
    Konrad, Charles
    ,
    Miller, Douglas
    ,
    Etherton, Brian
    DOI: 10.1175/2009BAMS2591.1
    Publisher: American Meteorological Society
    Abstract: Upslope-enhanced snowfall events during periods of northwesterly flow in the southern Appalachians have been recognized as a significant winter forecasting problem for some time. However, only in recent years has this problem received noteworthy attention by both the academic and operational communities. The complex meteorology of these events includes significant topographic influences, as well as a linkage between the upstream Great Lakes and resultant southern Appalachian snowfall. A unique collaborative team has recently formed, working toward the goals of improving the physical understanding of the mechanisms at work in these events and developing more accurate forecasts and more detailed climatologies. The literature shows only limited attention to this problem through the 1990s. However, with modernization of the National Weather Service (NWS) in the mid-1990s came opportunities to bring more attention to new or poorly understood forecast problems. These opportunities included the establishment of new forecast offices, often collocated with universities, the deployment of the Weather Surveillance Radar-1988 Doppler (WSR-88D) network, expansion of the surface observational network in both space and time, improved access to sophisticated numerical models, and growth of the spotter and cooperative observer networks. A collaborative team, consisting of faculty from five universities and meteorologists from six NWS forecast offices, has established an ongoing, structured dialogue to help advance the understanding and improve the forecasting of these events. The team utilizes a variety of communication strategies to discuss emerging research findings, review recent events, and share data and ideas. The ultimate goal is to continue fostering working relationships among research and operational meteorologists, climatologists, and students, all with a common motivation of continually improving forecasts and understanding of this important phenomenon. This group may serve as a model for other collaborative efforts between the research and operational communities interested in a common forecast problem.
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      A Collaborative Approach to Study Northwest Flow Snow in The Southern Appalachians

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209643
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    • Bulletin of the American Meteorological Society

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    contributor authorKeighton, Steve
    contributor authorLee, Laurence
    contributor authorHolloway, Blair
    contributor authorHotz, David
    contributor authorZubrick, Steven
    contributor authorHovis, Jeffrey
    contributor authorVotaw, Gary
    contributor authorPerry, L. Baker
    contributor authorLackmann, Gary
    contributor authorYuter, Sandra E.
    contributor authorKonrad, Charles
    contributor authorMiller, Douglas
    contributor authorEtherton, Brian
    date accessioned2017-06-09T16:27:12Z
    date available2017-06-09T16:27:12Z
    date copyright2009/07/01
    date issued2009
    identifier issn0003-0007
    identifier otherams-68120.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209643
    description abstractUpslope-enhanced snowfall events during periods of northwesterly flow in the southern Appalachians have been recognized as a significant winter forecasting problem for some time. However, only in recent years has this problem received noteworthy attention by both the academic and operational communities. The complex meteorology of these events includes significant topographic influences, as well as a linkage between the upstream Great Lakes and resultant southern Appalachian snowfall. A unique collaborative team has recently formed, working toward the goals of improving the physical understanding of the mechanisms at work in these events and developing more accurate forecasts and more detailed climatologies. The literature shows only limited attention to this problem through the 1990s. However, with modernization of the National Weather Service (NWS) in the mid-1990s came opportunities to bring more attention to new or poorly understood forecast problems. These opportunities included the establishment of new forecast offices, often collocated with universities, the deployment of the Weather Surveillance Radar-1988 Doppler (WSR-88D) network, expansion of the surface observational network in both space and time, improved access to sophisticated numerical models, and growth of the spotter and cooperative observer networks. A collaborative team, consisting of faculty from five universities and meteorologists from six NWS forecast offices, has established an ongoing, structured dialogue to help advance the understanding and improve the forecasting of these events. The team utilizes a variety of communication strategies to discuss emerging research findings, review recent events, and share data and ideas. The ultimate goal is to continue fostering working relationships among research and operational meteorologists, climatologists, and students, all with a common motivation of continually improving forecasts and understanding of this important phenomenon. This group may serve as a model for other collaborative efforts between the research and operational communities interested in a common forecast problem.
    publisherAmerican Meteorological Society
    titleA Collaborative Approach to Study Northwest Flow Snow in The Southern Appalachians
    typeJournal Paper
    journal volume90
    journal issue7
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/2009BAMS2591.1
    journal fristpage979
    journal lastpage991
    treeBulletin of the American Meteorological Society:;2009:;volume( 090 ):;issue: 007
    contenttypeFulltext
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