FURTHER STUDIES OF THERMALLY DRIVEN MOTIONS IN A ROTATING FLUIDSource: Journal of Meteorology:;1957:;volume( 014 ):;issue: 006::page 553Author:Kuo, H-L.
DOI: 10.1175/1520-0469(1957)014<0553:FSOTDM>2.0.CO;2Publisher: American Meteorological Society
Abstract: The transitions from the lower forced symmetric regime to the wave regime, within the wave regime itself and from the wave regime to the upper symmetric regime, are discussed by making use of the solution of a simplified version of the differential equation. It is found that the main features of these various transitions obtained by Fultz in some new experiments can be explained by the theories developed in this note and in the previous studies.
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| contributor author | Kuo, H-L. | |
| date accessioned | 2017-06-09T14:11:45Z | |
| date available | 2017-06-09T14:11:45Z | |
| date copyright | 1957/12/01 | |
| date issued | 1957 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14389.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149944 | |
| description abstract | The transitions from the lower forced symmetric regime to the wave regime, within the wave regime itself and from the wave regime to the upper symmetric regime, are discussed by making use of the solution of a simplified version of the differential equation. It is found that the main features of these various transitions obtained by Fultz in some new experiments can be explained by the theories developed in this note and in the previous studies. | |
| publisher | American Meteorological Society | |
| title | FURTHER STUDIES OF THERMALLY DRIVEN MOTIONS IN A ROTATING FLUID | |
| type | Journal Paper | |
| journal volume | 14 | |
| journal issue | 6 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1957)014<0553:FSOTDM>2.0.CO;2 | |
| journal fristpage | 553 | |
| journal lastpage | 558 | |
| tree | Journal of Meteorology:;1957:;volume( 014 ):;issue: 006 | |
| contenttype | Fulltext |