Electronic Resource
Springer
Boundary layer meteorology
1 (1970), S. 137-145
ISSN:
1573-1472
Source:
Springer Online Journal Archives 1860-2000
Topics:
Geosciences
,
Physics
Notes:
Abstract The equations for a family of wind spirals are derived with the assumption that the thermal wind in the friction layer decreases exponentially with increasing height. The results are discussed with reference to the flow in the planetary boundary layer over the Antarctic Plateau.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00185735
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