The two dimensional starting plume. November 1965. Wood, I. R. en_US 2021-11-25T12:42:56Z 2021-11-25T12:42:56Z 1965 en_US
dc.description.abstract Rate of advance and spread of either a two dimensional starting plume or a two dimensional density current on a vertical slope. The cap of the plume moves at 0.38 times the maximum velocity of the steady layer behind, and that the ratio of the length from the vertical origin to the to the leading edge of the cap to one half the maximum width of the cap is 3. The virtual mass concept is used to show that these two ratios are connected. en_US
dc.language English
dc.language.iso EN en_US
dc.publisher University of New South Wales - Water Research Laboratory en_US
dc.rights CC BY-NC-ND 3.0 en_US
dc.rights.uri en_US
dc.source Legacy MARC en_US
dc.source WRL Digitisation
dc.subject.other turbulence en_US
dc.subject.other turbulent flow en_US
dc.subject.other 2nd Australian Conference on Hydraulics and Fluid Mechanics en_US
dc.title The two dimensional starting plume. November 1965. en_US
dc.type Report en
dcterms.accessRights open access
dspace.entity.type Publication en_US
unsw.description.notePublic Supplementary notes: Offprint from conference paper. en_US
unsw.identifier.doi en_US
unsw.relation.faculty Engineering
unsw.relation.ispartofreportnumber UNSW Water Research Laboratory Report No. 72 en_US
unsw.relation.originalPublicationAffiliation Wood, I. R., Water Research Laboratory, Faculty of Engineering, UNSW en_US School of Civil and Environmental Engineering *
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