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Some observed properties of medium-scale diffusion in the atmosphere

โœ Scribed by F. Pasquill


Publisher
John Wiley and Sons
Year
1962
Tongue
English
Weight
731 KB
Volume
88
Category
Article
ISSN
0035-9009

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โœฆ Synopsis


Abstract

Diffusion experiments using fluorescent particles are described and data on travel and horizontal spread over distances 10 to 80 miles are summarized.

Good vertical mixing evidently counteracts the tendency for a cloud of particles to be sheared according to the wind profile. The effective velocity of the cloud is then close to the mean velocity through the layer of mixing, but some unexplained discrepancies in direction have been encountered. The shearing which can occur in the absence of vertical mixing will become effective as a horizontal spread through the action of subsequent vertical mixing.

The data are insufficient to allow any general conclusion to be reached about the relative importance of horizontal turbulence and vertical shear in promoting horizontal spread.


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