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contributor authorLong, Robert R.
date accessioned2017-06-09T14:11:22Z
date available2017-06-09T14:11:22Z
date copyright1956/02/01
date issued1956
identifier issn0095-9634
identifier otherams-14229.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149767
description abstractThe differential equations governing the unsteady motion of a system of two superimposed liquids are integrated by use of the method of characteristics. The solution differs significantly from that obtained by assuming a very thin lower layer. If the basic shear across the interface is small, a wave breaks forward (as an ordinary water wave) only if the amplitude is fairly small and if the lower layer is thinner than the upper layer. If the upper fluid is thinner, the wave breaks backward. The speed of the various points of the wave does not vary monotonically with amplitude. If a shear exists, higher velocities in the upper layer in the direction of wave propagation favor the forward breaking of a wave. The opposite shear may cause a wave to break backward.
publisherAmerican Meteorological Society
titleLONG WAVES IN A TWO-FLUID SYSTEM
typeJournal Paper
journal volume13
journal issue1
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1956)013<0070:LWIATF>2.0.CO;2
journal fristpage70
journal lastpage74
treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 001
contenttypeFulltext


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