| contributor author | Donn, William L. | |
| contributor author | Milic, Patricia L. | |
| contributor author | Brilliant, Renee | |
| date accessioned | 2017-06-09T14:11:30Z | |
| date available | 2017-06-09T14:11:30Z | |
| date copyright | 1956/08/01 | |
| date issued | 1956 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14279.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149822 | |
| description abstract | The dominant atmospheric pressure oscillations recorded by a microbarovariograph at Guantanamo Bay, Cuba, are explained as perturbations from internal gravity waves on the sea-breeze interface, aloft. The variograph traces have been analyzed statistically to demonstrate that they give a consistent reaction to the same phenomena. The surface and upper-air data have been utilized to show that the sea breeze is the cause of this consistent pattern. From the combination of these factors, a theoretical picture of the conditions necessary to the propagation of gravity waves on the sea-breeze inversion has been derived. | |
| publisher | American Meteorological Society | |
| title | GRAVITY WAVES AND THE TROPICAL SEA BREEZE | |
| type | Journal Paper | |
| journal volume | 13 | |
| journal issue | 4 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1956)013<0356:GWATTS>2.0.CO;2 | |
| journal fristpage | 356 | |
| journal lastpage | 361 | |
| tree | Journal of Meteorology:;1956:;volume( 013 ):;issue: 004 | |
| contenttype | Fulltext | |
