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contributor authorTyson, P. D.
date accessioned2017-06-09T14:14:25Z
date available2017-06-09T14:14:25Z
date copyright1968/05/01
date issued1968
identifier issn0022-4928
identifier otherams-15428.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151099
description abstractHorizontal 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.
publisherAmerican Meteorological Society
titleVelocity Fluctuations in the Mountain Wind
typeJournal Paper
journal volume25
journal issue3
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<0381:VFITMW>2.0.CO;2
journal fristpage381
journal lastpage384
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 003
contenttypeFulltext


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