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dc.contributor.authorShetye, S.R.
dc.date.accessioned2009-01-10T11:35:48Z
dc.date.available2009-01-10T11:35:48Z
dc.date.issued1999
dc.identifier.citationContinental Shelf Research, Vol.19; 1771-1782p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/1823
dc.description.abstractIn the Gulf of Kutch on the northwestern shelf of India the semi-diurnal constituents M sub(2) and S sub(2) get amplified approximately threefold. In contrast, amplification on the diurnal consituents K sub(1) and O sub(1) is small. From analytical and numerical solutions of linear, viscous, cross-sectionally averaged equations for tidal motion in a channel, it is seen that the observed amplification results from a combination of quarter-wavelength resonance, geometric effect due to decrease in width of the channel, and friction
dc.language.isoen
dc.publisherPergamon
dc.rightsCopyright [1999]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjecttides
dc.subjecttidal waves
dc.subjectwave length
dc.subjectnumerical analysis
dc.subjectmodels
dc.subjecttidal resonance
dc.titleTides in the Gulf of Kutch, India
dc.typeJournal Article


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