Velocity Fluctuations in the Mountain Wind
- 1 May 1968
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 25 (3) , 381-384
- https://doi.org/10.1175/1520-0469(1968)025<0381:vfitmw>2.0.co;2
Abstract
Horizontal velocity spectra of the mountain wind show that maximum turbulent energy is generated by waves the order of 10 km in length and a period of 1 hr, thereby filling the spectral gap between purely micrometeorological fluctuations on the one hand, and mesometeorological on the other.Keywords
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