Hailstorms and Hail Suppression Techniques in the U.S.S.R.—Source: Bulletin of the American Meteorological Society:;1973:;volume( 054 ):;issue: 004::page 317Author:Marwitz, John D.
DOI: 10.1175/1520-0477(1973)054<0317:HAHSTI>2.0.CO;2Publisher: 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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contributor author | Marwitz, John D. | |
date accessioned | 2017-06-09T14:39:14Z | |
date available | 2017-06-09T14:39:14Z | |
date copyright | 1973/04/01 | |
date issued | 1973 | |
identifier issn | 0003-0007 | |
identifier other | ams-23682.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4160270 | |
description 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. | |
publisher | American Meteorological Society | |
title | Hailstorms and Hail Suppression Techniques in the U.S.S.R.— | |
type | Journal Paper | |
journal volume | 54 | |
journal issue | 4 | |
journal title | Bulletin of the American Meteorological Society | |
identifier doi | 10.1175/1520-0477(1973)054<0317:HAHSTI>2.0.CO;2 | |
journal fristpage | 317 | |
journal lastpage | 325 | |
tree | Bulletin of the American Meteorological Society:;1973:;volume( 054 ):;issue: 004 | |
contenttype | Fulltext |