| contributor author | HUGHES, PATRICK E. | |
| contributor author | WOOD, RICHARD A. | |
| date accessioned | 2017-06-09T15:57:00Z | |
| date available | 2017-06-09T15:57:00Z | |
| date copyright | 1962/03/01 | |
| date issued | 1962 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-57280.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4197598 | |
| description abstract | Previous discussions of the ?bright band,? a radar phenomenon associated with the freezing level, have treated it as related to a ?normal? lapse rate?a progressive decrease of temperature with height, with surface temperatures above freezing. This paper deals with bright bands observed when surface temperatures were at, or below, freezing. Three cases are examined, all snowstorms of the 1960?61 season. In each case inspection of the available upper-air soundings confirmed the existence of prominent inversions aloft associated with the observed bright bands. | |
| publisher | American Meteorological Society | |
| title | THE INVERSION “BRIGHT BAND” | |
| type | Journal Paper | |
| journal volume | 90 | |
| journal issue | 3 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1962)090<0097:TIBB>2.0.CO;2 | |
| journal fristpage | 97 | |
| journal lastpage | 102 | |
| tree | Monthly Weather Review:;1962:;volume( 090 ):;issue: 003 | |
| contenttype | Fulltext | |
