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dc.contributor.authorHershey, Allen V.
dc.date1987-09
dc.date.accessioned2013-03-07T21:52:32Z
dc.date.available2013-03-07T21:52:32Z
dc.date.issued1987-09
dc.identifier.urihttp://hdl.handle.net/10945/29815
dc.description.abstractAny discontinuity in flov; at a plane boundary is dispersed by the diffusion of vorticity into a boundary layer and vyake. Experimental measurements in the past have been correlated with empirical formulations. A generalization gives both the horizontal component and the vertical component of the mean velocity. In the laminar sublayer the velocity is a solution of the diffusion equation. In the turbulent boundary layer the velocity can be expressed by a Fourier integral. In the free stream there is a vertical persistence of velocity. The computation of velocity is provided by subroutines.en_US
dc.description.sponsorshipPrepared for: Naval Postgraduate School Monterey, CAen_US
dc.description.urihttp://archive.org/details/diffusionofvorti00hers
dc.language.isoen_US
dc.publisherMonterey, California. Naval Postgraduate Schoolen_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, may not be copyrighted.en_US
dc.subject.lcshCONDENSERS (STEAM)en_US
dc.titleThe diffusion of vorticity from a plane boundaryen_US
dc.typeTechnical Reporten_US
dc.contributor.corporateNaval Postgraduate School (U.S.)
dc.subject.authorFourier Analysisen_US
dc.subject.authorNumerical Analysisen_US
dc.subject.authorHydrodynamicsen_US
dc.description.recognitionNAen_US
dc.identifier.oclcNA
dc.identifier.npsreportNPS-012-87-006


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