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    Hailstorms and Hail Suppression Techniques in the U.S.S.R.—

    Source: Bulletin of the American Meteorological Society:;1973:;volume( 054 ):;issue: 004::page 317
    Author:
    Marwitz, John D.
    DOI: 10.1175/1520-0477(1973)054<0317:HAHSTI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper reports the results from the latest in a series of scientific exchanges concerning the Soviet anti-hail program. Additional details on the Soviet technique of hail suppression were learned. An impression on the types of storms and the accompanying synoptic conditions was gained. In addition to visual impressions, some case studies are presented. The North Caucasus region resembles northeastern Colorado from a topographical and meteorological point of view, except that a dry line or dew-point front is not normally present north of the Caucasus Mountains. The abundance of low-level moisture in this region seems to produce storms which resemble cloud streets in that lines of storms are aligned with the wind rather than normal to the wind. Although the large supercell and multicell storms typical of the High Plains of North America do occur in the Caucasus region, they are rare and the Soviet scientists are apparently unable to suppress all the hail on these types of storms.
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      Hailstorms and Hail Suppression Techniques in the U.S.S.R.—

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4160270
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    contributor authorMarwitz, John D.
    date accessioned2017-06-09T14:39:14Z
    date available2017-06-09T14:39:14Z
    date copyright1973/04/01
    date issued1973
    identifier issn0003-0007
    identifier otherams-23682.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160270
    description abstractThis paper reports the results from the latest in a series of scientific exchanges concerning the Soviet anti-hail program. Additional details on the Soviet technique of hail suppression were learned. An impression on the types of storms and the accompanying synoptic conditions was gained. In addition to visual impressions, some case studies are presented. The North Caucasus region resembles northeastern Colorado from a topographical and meteorological point of view, except that a dry line or dew-point front is not normally present north of the Caucasus Mountains. The abundance of low-level moisture in this region seems to produce storms which resemble cloud streets in that lines of storms are aligned with the wind rather than normal to the wind. Although the large supercell and multicell storms typical of the High Plains of North America do occur in the Caucasus region, they are rare and the Soviet scientists are apparently unable to suppress all the hail on these types of storms.
    publisherAmerican Meteorological Society
    titleHailstorms and Hail Suppression Techniques in the U.S.S.R.—
    typeJournal Paper
    journal volume54
    journal issue4
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1973)054<0317:HAHSTI>2.0.CO;2
    journal fristpage317
    journal lastpage325
    treeBulletin of the American Meteorological Society:;1973:;volume( 054 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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