| contributor author | Austin, J. M. | |
| contributor author | Shapiro, R. | |
| date accessioned | 2017-06-09T14:10:24Z | |
| date available | 2017-06-09T14:10:24Z | |
| date copyright | 1951/06/01 | |
| date issued | 1951 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-13834.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149328 | |
| description abstract | The hypothesis is investigated that there is a physical difference between the development and motion components of a surface pressure change. Temperature changes indicate that deepening and filling are accompanied by high-level heating and cooling, respectively, while the motion part of pressure changes is associated with low-level temperature variations. | |
| publisher | American Meteorological Society | |
| title | TROPOSPHERIC AND STRATOSPHERIC TEMPERATURE CHANGES ASSOCIATED WITH PRESSURE CHANGES | |
| type | Journal Paper | |
| journal volume | 8 | |
| journal issue | 3 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1951)008<0191:TASTCA>2.0.CO;2 | |
| journal fristpage | 191 | |
| journal lastpage | 195 | |
| tree | Journal of Meteorology:;1951:;volume( 008 ):;issue: 003 | |
| contenttype | Fulltext | |
