DISSIPATION OF STRATUS CLOUDS IN A TURBULENT ATMOSPHERE
AMERICAN METEOROLOGICAL SOCIETY BOSTON MA BOSTON United States
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The report contains the horizontal dissipation of a spatially homogeneous stratus cloud in a turbulent atmosphere, in which isothermy, an inversion in the supracloud layer, and downdrafts are present the time required for total dissipation of the cloud is computed.
- Atmospheric Physics