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dc.contributor.authorReddy, G.V.
dc.contributor.authorSastry, J.S.
dc.date.accessioned1995-08-27T10:01:43Z
dc.date.accessioned2017-09-30T01:29:42Z
dc.date.available1995-08-27T10:01:43Z
dc.date.available2017-09-30T01:29:42Z
dc.date.issued1988
dc.identifier.citationMahasagar, vol.21; 1988; 125-133
dc.identifier.issn0542-0938
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6967
dc.description.abstractRemoval of sand by wind from the beach at Miramar-Caranzalem, Goa, has been found to effect its stability over a relatively longer time scale. This aeolian sand transport has been computed for this strip of the beach utilising the relation between the rate of sediment transport, the sediment and wind characteristics. The winds recorded at Panaji for the period 1969-1973 have been analysed and discussed for the directional transport of sand from the beachface. During fair weather months, the diurnal, inland, aeolian transport has been found to be nearly 180 m3 per km. length of the beach subjected to 10 m/sec, winds lasting for periods of approximately 8 hrs. a day. The resulting transport and its effects on the stability of this beach has been discussed
dc.languageen
dc.publisherIndian Association for Limnology and Oceanography
dc.relation.ispartofMahasagar
dc.relation.isreferencedbyNON-SCI
dc.subjectGeology and Geophysics
dc.subject.otherwinds
dc.subject.otherbeaches
dc.subject.othersediment stability
dc.subject.otheraeolian transport
dc.subject.otherISW, India, Goa, Miramar-Caranzalem beach
dc.titleAeolian sand transport and its effects on the stability of Miramar-Caranzalem beach
dc.typeJournal Article


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