Bulletin of the American Meteorological Society, Volumen82American Meteorological Society., 2001 List of members in v. 1, 8. |
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... convection outside the eyewall cloud . Less ( more ) convection in this zone leads to a lower ( higher ) central pressure and smaller ( larger ) radii of 50 - kt ( approximately 26 m s ̄1 ) and 30 - kt ( approximately 15 m s ̄1 ) ...
... convection outside the eyewall cloud . Less ( more ) convection in this zone leads to a lower ( higher ) central pressure and smaller ( larger ) radii of 50 - kt ( approximately 26 m s ̄1 ) and 30 - kt ( approximately 15 m s ̄1 ) ...
Página 2219
... convection and positive in the weak phase of convection in the bay ; the observed Earlier studies suggest that atmospheric conditions have a significant impact on the SST of the bay . However , the extent to which variation of SST modu ...
... convection and positive in the weak phase of convection in the bay ; the observed Earlier studies suggest that atmospheric conditions have a significant impact on the SST of the bay . However , the extent to which variation of SST modu ...
Página 2223
... convection . 25 Normally air is not saturated to start with and a fi- nite vertical displacement ( a few hundred meters to a few kilometers ) is needed for the rising air parcel to become saturated and reach the level of free convec ...
... convection . 25 Normally air is not saturated to start with and a fi- nite vertical displacement ( a few hundred meters to a few kilometers ) is needed for the rising air parcel to become saturated and reach the level of free convec ...
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ARTICLES | 1993 |
Journal of Atmospheric Sciences | 2001 |
ARTICLES | 2105 |
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