Arizona Cool Season Surface Wind and Pressure Gradient StudySource: Bulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 002::page 114Author:Brenner, Ira S.
DOI: 10.1175/1520-0477(1980)061<0114:ACSSWA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The average sea-level pressure gradients that produce sustained surface winds above 8 kt for at least six consecutive hours during the cool season at predetermined key stations in or adjacent to Arizona are investigated. Only wind directions with northerly or easterly components are included in the developmental data sample. Graphs are provided that relate the derived pressure gradients to varying surface wind speeds at each key station.
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| contributor author | Brenner, Ira S. | |
| date accessioned | 2017-06-09T14:39:51Z | |
| date available | 2017-06-09T14:39:51Z | |
| date copyright | 1980/02/01 | |
| date issued | 1980 | |
| identifier issn | 0003-0007 | |
| identifier other | ams-23941.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4160558 | |
| description abstract | The average sea-level pressure gradients that produce sustained surface winds above 8 kt for at least six consecutive hours during the cool season at predetermined key stations in or adjacent to Arizona are investigated. Only wind directions with northerly or easterly components are included in the developmental data sample. Graphs are provided that relate the derived pressure gradients to varying surface wind speeds at each key station. | |
| publisher | American Meteorological Society | |
| title | Arizona Cool Season Surface Wind and Pressure Gradient Study | |
| type | Journal Paper | |
| journal volume | 61 | |
| journal issue | 2 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/1520-0477(1980)061<0114:ACSSWA>2.0.CO;2 | |
| journal fristpage | 114 | |
| journal lastpage | 121 | |
| tree | Bulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 002 | |
| contenttype | Fulltext |