| contributor author | Byers, Horace R. | |
| contributor author | Coons, Richard D. | |
| date accessioned | 2017-06-09T14:09:46Z | |
| date available | 2017-06-09T14:09:46Z | |
| date copyright | 1947/06/01 | |
| date issued | 1947 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-13579.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149044 | |
| description abstract | Observations on 10-cm height-finding radar of echoes from stratified clouds indicate a horziontal band which produces a stronger return than the parts above or below it. The height of ?bright line? occurrence is always at the freezing level and therefore supports the idea of drop formation and consequently radar-target formation in the colloidally unstable layer of heterogeneous ice-water mixture. Several examples are given from the thunderstorm observation network in the vicinity of Orlando, Florida | |
| publisher | American Meteorological Society | |
| title | THE ‘BRIGHT LINE’ IN RADAR CLOUD ECHOES AND ITS PROBABLE EXPLANATION | |
| type | Journal Paper | |
| journal volume | 4 | |
| journal issue | 3 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1947)004<0078:TLIRCE>2.0.CO;2 | |
| journal fristpage | 78 | |
| journal lastpage | 81 | |
| tree | Journal of Meteorology:;1947:;volume( 004 ):;issue: 003 | |
| contenttype | Fulltext | |
