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 s1 ) winds ...
... 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 s1 ) winds ...
Página 2223
... convection . 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- tion ...
... convection . 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- tion ...
Página 2234
... convection at TS2 . the surface air and the average CAPE exhibit similar temporal variation . The mean values of surface and average CAPE are around 3 and about 1 kJ kg ' , re- spectively . Values of CAPE are high before convec- tion ...
... convection at TS2 . the surface air and the average CAPE exhibit similar temporal variation . The mean values of surface and average CAPE are around 3 and about 1 kJ kg ' , re- spectively . Values of CAPE are high before convec- tion ...
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articles meeting summary | 1853 |
Evidence for Intensification of North Pacific Winter | 1869 |
The Ensemble of Tropical Cyclone Track | 1895 |
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