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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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