| contributor author | COLÓN, JOSÉ A. | |
| contributor author | NIGHTINGALE, WILLIAM R. | |
| date accessioned | 2017-06-09T15:57:18Z | |
| date available | 2017-06-09T15:57:18Z | |
| date copyright | 1963/07/01 | |
| date issued | 1963 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-57409.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4197742 | |
| description abstract | The 200-mb. flow existing above low-level perturbations at the time of development into tropical storm or hurricane intensity was studied. On the basis of observations in a sample of 40 cases, it is concluded that poleward flow aloft, such as is found in the eastern side of troughs in the westerlies and tropical upper-level cold Lows or in the western side of anticyclones, is more favorable for development of low-level perturbations underneath than equatorward flow. It is also shown that flow aloft with anticyclonic vorticity is more favorable than flow with cyclonic vorticity. | |
| publisher | American Meteorological Society | |
| title | DEVELOPMENT OF TROPICAL CYCLONES IN RELATION TO CIRCULATION PATTERNS AT THE 200-MILLIBAR LEVEL | |
| type | Journal Paper | |
| journal volume | 91 | |
| journal issue | 7 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1963)091<0329:DOTCIR>2.3.CO;2 | |
| journal fristpage | 329 | |
| journal lastpage | 336 | |
| tree | Monthly Weather Review:;1963:;volume( 091 ):;issue: 007 | |
| contenttype | Fulltext | |
