In:
Radio Science, American Geophysical Union (AGU), Vol. 4, No. 12 ( 1969-12), p. 1133-1136
Abstract:
An exponential relationship between the vertical wind shear and the layer thickness over which this shear is measured has been derived. From an analysis of the Richardson number it appears that shallow layers reaching maximum shearing conditions under the established power law should be turbulent, irrespective of the prevailing thermal stability conditions.
Type of Medium:
Online Resource
ISSN:
0048-6604
,
1944-799X
DOI:
10.1029/RS004i012p01133
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
1969
detail.hit.zdb_id:
2011445-X
SSG:
16,13