| dc.contributor.author | Brooks, H. B. | |
| dc.date.accessioned | 2017-06-09T14:12:17Z | |
| dc.date.available | 2017-06-09T14:12:17Z | |
| dc.date.copyright | 1960/02/01 | |
| dc.date.issued | 1960 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-14596.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150174 | |
| dc.description.abstract | The writer has observed that large dust devils rotate cyclonically, at least near Tucson, Arizona. This implies that the dust-devil is a central feature of a convective cell whose horizontal radius is frequently a mile. A graph of wind speed versus vortex radius is included. | |
| dc.publisher | American Meteorological Society | |
| dc.title | SHORTER CONTRIBUTIONS | |
| dc.type | Journal Paper | |
| dc.journal.volume | 17 | |
| dc.journal.issue | 1 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1960)017<0084:SC>2.0.CO;2 | |
| dc.journal.fristpage | 84 | |
| dc.journal.lastpage | 86 | |
| dc.tree | Journal of Meteorology:;1960:;volume( 017 ):;issue: 001 | |
| dc.contenttype | Fulltext | |
