NOTE ON ESTIMATION OF VERTICAL MOTION BY THE OMEGA EQUATIONSource: Monthly Weather Review:;1969:;volume( 097 ):;issue: 012::page 902Author:DJURIC, DUŠAN
DOI: 10.1175/1520-0493(1969)097<0902:NOEOVM>2.3.CO;2Publisher: American Meteorological Society
Abstract: An interpretation of the ?-equation shows that upward motion is closely related to the advection of vorticity in the upper troposphere and to warm advection in the lower troposphere. Examples are presented to illustrate both effects.
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| contributor author | DJURIC, DUŠAN | |
| date accessioned | 2017-06-09T15:59:11Z | |
| date available | 2017-06-09T15:59:11Z | |
| date copyright | 1969/12/01 | |
| date issued | 1969 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-58152.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4198568 | |
| description abstract | An interpretation of the ?-equation shows that upward motion is closely related to the advection of vorticity in the upper troposphere and to warm advection in the lower troposphere. Examples are presented to illustrate both effects. | |
| publisher | American Meteorological Society | |
| title | NOTE ON ESTIMATION OF VERTICAL MOTION BY THE OMEGA EQUATION | |
| type | Journal Paper | |
| journal volume | 97 | |
| journal issue | 12 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1969)097<0902:NOEOVM>2.3.CO;2 | |
| journal fristpage | 902 | |
| journal lastpage | 904 | |
| tree | Monthly Weather Review:;1969:;volume( 097 ):;issue: 012 | |
| contenttype | Fulltext |