Friday, 26 May 2000: 4:00 PM
In this work, we use data collected during the intensive operation
period of TOGA-COARE to study, on a case-by-case basis, the nature of moisture
interchange between cloud systems and their environment. For our ten-case sample, we have
found a correlation between cloud-top height and mid-level moisture. We also argue
that it is mid-level moisture which is controlling the height of the clouds
and not vice-versa. Furthermore, by using the stochastic mixing model, Raymond and
Blyth (1992), we obtained evidence that entrainment is a plausible mechanism to
explain how mid-level moisture exercises such a control.
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