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contributor authorChing, Jason K. S.
contributor authorBusinger, J. A.
date accessioned2017-06-09T14:14:40Z
date available2017-06-09T14:14:40Z
date copyright1968/11/01
date issued1968
identifier issn0022-4928
identifier otherams-15523.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151205
description abstractThe equations for horizontally homogeneous planetary boundary layer flow with constant eddy viscosity are integrated in time and height. The special case for which the direction of the pressure gradient force is a periodic function of time is studied in detail. The nondimensional number F=z(4Kt)?½ is seen to be the proper scale which describes the flow response to the boundary layer.
publisherAmerican Meteorological Society
titleThe Response of the Planetary Boundary Layer to Time Varying Pressure Gradient Force
typeJournal Paper
journal volume25
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<1021:TROTPB>2.0.CO;2
journal fristpage1021
journal lastpage1025
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006
contenttypeFulltext


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