A refined view of vertical transport by cumulus convection
The purpose of this letter is to show that the traditional view of transport by shallow cumulus clouds needs important refinement. On the basis of a straightforward geometrical analysis of Large Eddy Simulation results of shallow cumulus clouds, we conclude (1) that the upward mass transport by clouds is strongly dominated by regions close to the edge of clouds rather than by the core region of clouds and (2) that the downward mass transport is dominated by processes just outside the cloud. The latter finding contradicts the accepted view of a uniformly descending dry environment. We therefore advocate a refined view which distinguishes between the near-cloud environment and the distant environment. The near-cloud environment is characterized by coherent descending motions, whereas the distant environment is rather quiescent and plays no significant role in vertical transport.
document
http://n2t.net/ark:/85065/d7js9rrd
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2008-04-05T00:00:00Z
An edited version of this paper was published by AGU. Copyright 2008 American Geophysical Union.
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