| dc.contributor.author | Langwell, Patricia A. | |
| dc.date.accessioned | 2017-06-09T14:10:44Z | |
| dc.date.available | 2017-06-09T14:10:44Z | |
| dc.date.copyright | 1953/06/01 | |
| dc.date.issued | 1953 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-13983.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149493 | |
| dc.description.abstract | The cumuli which form over the ocean near Puerto Rico cannot be the result of ?thermals.? A theory is evolved, based on the oscillation of the boundary between the well-mixed layer near the ocean and the cloud layer. The physical plausibility of this theory is investigated by a development of stability criteria from the frequency equation. | |
| dc.publisher | American Meteorological Society | |
| dc.title | A MECHANISM FOR CONVECTION OVER THE OCEAN | |
| dc.type | Journal Paper | |
| dc.journal.volume | 10 | |
| dc.journal.issue | 3 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1953)010<0187:AMFCOT>2.0.CO;2 | |
| dc.journal.fristpage | 187 | |
| dc.journal.lastpage | 190 | |
| dc.tree | Journal of Meteorology:;1953:;volume( 010 ):;issue: 003 | |
| dc.contenttype | Fulltext | |
