| dc.contributor.author | Jordan, Elizabeth S. | |
| dc.date.accessioned | 2017-06-09T14:10:36Z | |
| dc.date.available | 2017-06-09T14:10:36Z | |
| dc.date.copyright | 1952/10/01 | |
| dc.date.issued | 1952 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-13928.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149432 | |
| dc.description.abstract | All available rawin-reports taken within the circulation of tropical storms are combined to obtain a generalized pattern of the upper wind-circulation. The cyclonic circulation decreases rapidly with height, and by 45,000 ft the circulation is anticyclonic beyond 3 deg lat from the center. The relative vorticity in the upper troposphere is found to be negative and great enough in magnitude so that zero absolute vorticity is approached. | |
| dc.publisher | American Meteorological Society | |
| dc.title | AN OBSERVATIONAL STUDY OF THE UPPER WIND-CIRCULATION TROPICAL STORMS | |
| dc.type | Journal Paper | |
| dc.journal.volume | 9 | |
| dc.journal.issue | 5 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1952)009<0340:AOSOTU>2.0.CO;2 | |
| dc.journal.fristpage | 340 | |
| dc.journal.lastpage | 346 | |
| dc.tree | Journal of Meteorology:;1952:;volume( 009 ):;issue: 005 | |
| dc.contenttype | Fulltext | |
