Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/37557
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dc.contributor.authorChandramohan, P-
dc.contributor.authorNayak, B U-
dc.contributor.authorKumar, V Sanil-
dc.contributor.authorPathak, K C-
dc.date.accessioned2016-11-25T05:01:21Z-
dc.date.available2016-11-25T05:01:21Z-
dc.date.issued1994-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/37557-
dc.description102-104en_US
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.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.23(2) [June 1994]en_US
dc.titleBeach processes between Mulgund and Shiroda, west coast of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.23(2) [June 1994]

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