Bulletin of the American Meteorological Society, Volumen78,Temas9-12American Meteorological Society, 1997 List of members in v. 1, 8. |
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Página 2185
... layer rapidly in a vertically divergent fashion , producing a decreased concentration of particles below the melt- ing layer . These factors combine to produce a pro- nounced bright band of enhanced reflectivity in a shal- low layer ...
... layer rapidly in a vertically divergent fashion , producing a decreased concentration of particles below the melt- ing layer . These factors combine to produce a pro- nounced bright band of enhanced reflectivity in a shal- low layer ...
Página 2192
... layer of maximum convergence in the upper troposphere corresponding to the convergence at the base of the elevated , hori- zontally spreading buoyant elements . This hypotheti- cal profile of divergence is consistent with the observed ...
... layer of maximum convergence in the upper troposphere corresponding to the convergence at the base of the elevated , hori- zontally spreading buoyant elements . This hypotheti- cal profile of divergence is consistent with the observed ...
Página 2632
... layer where turbulent interaction takes place.13 This prob- lematical aspect of the theory seems to have been an ... layer " into meteorology in his textbook on atmospheric turbulence ( Lettau 1939 , sect . 29 ) . This layer couples the ...
... layer where turbulent interaction takes place.13 This prob- lematical aspect of the theory seems to have been an ... layer " into meteorology in his textbook on atmospheric turbulence ( Lettau 1939 , sect . 29 ) . This layer couples the ...
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