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dc.contributor.authorChandramohan, P.
dc.contributor.authorNayak, B.U.
dc.contributor.authorSanilKumar, V.
dc.contributor.authorPathak, K.C.
dc.date.accessioned1994-07-13T10:06:26Z
dc.date.accessioned2017-09-30T02:52:21Z
dc.date.available1994-07-13T10:06:26Z
dc.date.available2017-09-30T02:52:21Z
dc.date.issued1994
dc.identifier.citationIndian Journal of Marine Sciences, vol.23(2); 1994; 102-104
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7473
dc.description.abstractStudy on beach processes for an year shows seasonal changes without annual net erosion. The beaches are stable and regain the maximum profiles during February to April. Distribution of longshore current direction is not uniform along the study region indicating the presence of variable littoral transport environment. This region is subjected to relatively low wave energy during the non-monsoon period
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.otherbeaches
dc.subject.otherlongshore currents
dc.subject.othersediments
dc.subject.othertemporal variations
dc.subject.otherISW, India, West Coast
dc.titleBeach processes between Mulgund and Shiroda, west coast of India
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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