Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/34455
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dc.contributor.authorChavan, S S-
dc.contributor.authorSawant, M D-
dc.contributor.authorChandra, Prabhat-
dc.contributor.authorNagendra, T-
dc.date.accessioned2016-06-27T04:49:19Z-
dc.date.available2016-06-27T04:49:19Z-
dc.date.issued2014-07-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/34455-
dc.description1364-1369en_US
dc.description.abstractBarrage is to utilize the fresh water on the u/s side of barrage and also to prevent the mixing of saline water during non-monsoon by fully closing the gates. During the monsoon season, the salinity of the water in Valvanta River becomes very low of about less than 5 ppt due to the predominant effect of River discharges. These types of studies are very vital for the water harnessing projects particularly on Western Ghats where the short estuaries drain into the sea without the water being utilized much. In the present study, is an attempt to predict the changes in the hydrodynamic conditions in the downstream side of barrage at Virdi by using the 1-D model HEC – RAS for different operational and tidal conditions.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.43(7) [July 2014]en_US
dc.subjectBarrageen_US
dc.subjectTidal reflectionen_US
dc.subjectSubmergenceen_US
dc.subjectWater levelen_US
dc.subjectCurrenten_US
dc.titleEffect of barrages on water level in estuariesen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.43(07) [July 2014]

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