Bulletin of the American Meteorological Society, Volúmenes38-39;Volúmenes38-39American Meteorological Society, 1957 Vols. for 1990- contain supplemental membership directory. |
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Página 223
... geostrophic wind , averaged over at least 8 mb when possible , was computed . A thickness line was assumed to move in the direction , and with the speed , of the initial geostrophic wind for 12 hours . K was then taken as the ratio of ...
... geostrophic wind , averaged over at least 8 mb when possible , was computed . A thickness line was assumed to move in the direction , and with the speed , of the initial geostrophic wind for 12 hours . K was then taken as the ratio of ...
Página 285
... wind maximum exceeds the wind speed at the level of the next higher minimum by 5 knots or more . ALTITUDE ( FEET ) 8000 7000 4000 6000 Mean Gradient Wind Speed- 1500 RELATION TO THE GEOSTROPHIC WIND During the hours after sunset , the ...
... wind maximum exceeds the wind speed at the level of the next higher minimum by 5 knots or more . ALTITUDE ( FEET ) 8000 7000 4000 6000 Mean Gradient Wind Speed- 1500 RELATION TO THE GEOSTROPHIC WIND During the hours after sunset , the ...
Página 289
... wind vector V ( † ) to the initial values W. , V. , and the geostrophic wind vector V ,, during a frictionally initiated inertia oscillation . distribution of wind with height , one may predict the entire wind distribution at a later ...
... wind vector V ( † ) to the initial values W. , V. , and the geostrophic wind vector V ,, during a frictionally initiated inertia oscillation . distribution of wind with height , one may predict the entire wind distribution at a later ...
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