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    UPSLOPE WEATHER ALONG THE INLAND ALASKA AIR ROUTE

    Source: Journal of Meteorology:;1944:;volume( 001 ):;issue: 003::page 98
    Author:
    Kolb, Louis L.
    ,
    Goodmanson, Murel M.
    DOI: 10.1175/1520-0469(1944)001<0098:UWATIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The importance of upslope circulation and its accompanying weather phenomena is discussed as a major factor influencing aircraft operation along the portion of the Inland Alaska Air Route which lies east of the Rocky Mountains. Great Falls, Montana, is given the greatest consideration since it is considered as representative of stations on the east slopes of the Rocky Mountains and more data are available for this station. The air masses involved in the occurrence of upslope circulation and associated phenomena are ascertained. Upslope weather types are classified into pure upslope, upslope?overrunning, upslope?radiation, and overrunning predominant with upslope as a minor factor. These types are correlated with typical synoptic examples. Forecasting of the formation and cessation of upslope weather phenomena is discussed on the basis of lower-air trajectories and the use of typical examples. Concrete deductions resulting from a study of many synoptic situations are enumerated as an aid in forecasting the formation and cessation of these phenomena.
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      UPSLOPE WEATHER ALONG THE INLAND ALASKA AIR ROUTE

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4148984
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    • Journal of Meteorology

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    contributor authorKolb, Louis L.
    contributor authorGoodmanson, Murel M.
    date accessioned2017-06-09T14:09:36Z
    date available2017-06-09T14:09:36Z
    date copyright1944/12/01
    date issued1944
    identifier issn0095-9634
    identifier otherams-13524.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148984
    description abstractThe importance of upslope circulation and its accompanying weather phenomena is discussed as a major factor influencing aircraft operation along the portion of the Inland Alaska Air Route which lies east of the Rocky Mountains. Great Falls, Montana, is given the greatest consideration since it is considered as representative of stations on the east slopes of the Rocky Mountains and more data are available for this station. The air masses involved in the occurrence of upslope circulation and associated phenomena are ascertained. Upslope weather types are classified into pure upslope, upslope?overrunning, upslope?radiation, and overrunning predominant with upslope as a minor factor. These types are correlated with typical synoptic examples. Forecasting of the formation and cessation of upslope weather phenomena is discussed on the basis of lower-air trajectories and the use of typical examples. Concrete deductions resulting from a study of many synoptic situations are enumerated as an aid in forecasting the formation and cessation of these phenomena.
    publisherAmerican Meteorological Society
    titleUPSLOPE WEATHER ALONG THE INLAND ALASKA AIR ROUTE
    typeJournal Paper
    journal volume1
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1944)001<0098:UWATIA>2.0.CO;2
    journal fristpage98
    journal lastpage108
    treeJournal of Meteorology:;1944:;volume( 001 ):;issue: 003
    contenttypeFulltext
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