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Instability of Time‐Periodic Flows of Stratified Fluids

dc.contributor.authorLi, Chin‐Hsiuen_US
dc.date.accessioned2010-05-06T21:39:07Z
dc.date.available2010-05-06T21:39:07Z
dc.date.issued1970-05en_US
dc.identifier.citationLi, Chin‐Hsiu (1970). "Instability of Time‐Periodic Flows of Stratified Fluids." Physics of Fluids 13(5): 1121-1134. <http://hdl.handle.net/2027.42/70112>en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/70112
dc.description.abstractThe instability of two liquid layers with a free surface set in motion by an oscillatory lower boundary is analyzed for two superposed fluids with different viscosities and different densities. There are two modes of wave motion: the interfacial and the free‐surface modes. When the Froude number is less than about 3, the interfacial mode governs the instability of the flow. For this case the free‐surface mode is always stable. The two surfaces of discontinuity are always in the phase for the free‐surface mode of disturbance, but may be in phase or 180 deg out of phase for the interfacial mode. The two modes, however, are found to compete with each other for governing the instability of the flow when the Froude number is larger than 3. The two surfaces of discontinuity can be out of phase by an angle different from 180 deg.en_US
dc.format.extent3102 bytes
dc.format.extent933404 bytes
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dc.format.mimetypeapplication/pdf
dc.publisherThe American Institute of Physicsen_US
dc.rights© The American Institute of Physicsen_US
dc.titleInstability of Time‐Periodic Flows of Stratified Fluidsen_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Engineering Mechanics, The University of Michigan Ann Arbor, Michiganen_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/70112/2/PFLDAS-13-5-1121-1.pdf
dc.identifier.doi10.1063/1.1693041en_US
dc.identifier.sourcePhysics of Fluidsen_US
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dc.owningcollnamePhysics, Department of


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