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The role of convection in surface property and velocity fluctuations

✍ Scribed by S. L. Ulanski; R. K. Hadlock; M. Garstang


Publisher
Springer
Year
1974
Tongue
English
Weight
617 KB
Volume
6
Category
Article
ISSN
0006-8314

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A simple model is deduced for the surface layer of a convective boundary layer for zero mean wind velocity over homogeneous rough ground. The model assumes large-scale convective circulation driven by surface heat flux with a flow pattern as it would be obtained by conditional ensemble averages. The