RADAR DETECTION OF A FRONTAL STORM 18 JUNE 1946Source: Journal of Meteorology:;1947:;volume( 004 ):;issue: 001::page 38Author:Wexler, Raymond
DOI: 10.1175/1520-0469(1947)004<0038:RDOAFS>2.0.CO;2Publisher: American Meteorological Society
Abstract: The theory of radar storm detection is briefly stated and applied to detection of the frontal storm of 18 June 1946. The precipitation pattern associated with the front is found to be a series of overlapping line squalls each about 100 miles in length. The mean rain intensity along the front is computed with the aid of radar theory.
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| contributor author | Wexler, Raymond | |
| date accessioned | 2017-06-09T14:09:45Z | |
| date available | 2017-06-09T14:09:45Z | |
| date copyright | 1947/02/01 | |
| date issued | 1947 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-13567.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149031 | |
| description abstract | The theory of radar storm detection is briefly stated and applied to detection of the frontal storm of 18 June 1946. The precipitation pattern associated with the front is found to be a series of overlapping line squalls each about 100 miles in length. The mean rain intensity along the front is computed with the aid of radar theory. | |
| publisher | American Meteorological Society | |
| title | RADAR DETECTION OF A FRONTAL STORM 18 JUNE 1946 | |
| type | Journal Paper | |
| journal volume | 4 | |
| journal issue | 1 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1947)004<0038:RDOAFS>2.0.CO;2 | |
| journal fristpage | 38 | |
| journal lastpage | 44 | |
| tree | Journal of Meteorology:;1947:;volume( 004 ):;issue: 001 | |
| contenttype | Fulltext |