| contributor author | Milliff, Ralph F. | |
| contributor author | Madden, Roland A. | |
| date accessioned | 2017-06-09T14:33:43Z | |
| date available | 2017-06-09T14:33:43Z | |
| date copyright | 1996/02/01 | |
| date issued | 1996 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-21702.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4158071 | |
| description abstract | Eastward phase propagation, at speed faster than 30 m s?1, of a signal in the equatorial troposphere of the Eastern Pacific is detected, first in historical meteorological observations and then in more recent data. A first baroclinic mode vertical structure is identified with this signal in separate analyses based on linear theory and complex empirical orthogonal functions, respectively. This rapid, eastward signal is conceptualized as a far-field dispersion product of strong convection associated with the intraseasonal tropical oscillation in the Indian Ocean and Western Pacific. | |
| publisher | American Meteorological Society | |
| title | The Existence and Vertical Structure of Fast, Eastward-Moving Disturbances in the Equatorial Troposphere | |
| type | Journal Paper | |
| journal volume | 53 | |
| journal issue | 4 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1996)053<0586:TEAVSO>2.0.CO;2 | |
| journal fristpage | 586 | |
| journal lastpage | 597 | |
| tree | Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 004 | |
| contenttype | Fulltext | |