Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/42599
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dc.contributor.authorKomijani, Fereshteh-
dc.date.accessioned2017-08-11T05:25:47Z-
dc.date.available2017-08-11T05:25:47Z-
dc.date.issued2017-09-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/42599-
dc.description1848-1859en_US
dc.description.abstractMazandaran coast, can be classified into three wave-dominated beach types. Moderate to high rips stability (and risk) of transient and topographic rips are generated in eastern and central coasts, respectively, which are a product of dissipative and intermediate modes, wave hydrodynamics, sediment conditions and beach morphology. Generation of morphologically controlled rips in central Mazandaran can result in a permanent threat because of a fixed alongshore non-uniform bathymetry. Transient rips in eastern coasts is a product of dissipative mode with flat bathymetry. However, a uniform and steep beach bottom causes strong Backwash along reflective western coast. On the average, all Mazandaran coasts maintain their beach states seasonally with only small changes in morphodynamic 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.46(09) [September 2017]en_US
dc.subjectCaspian Seaen_US
dc.subjectMazandaran coastsen_US
dc.subjectRip Currenten_US
dc.subjectBeach Stateen_US
dc.subjectWave Hydrodynamicsen_US
dc.subjectBed Morphologyen_US
dc.titleControls on the occurrence of various types of rip current along the Mazandaran Coast –Southern Caspian Seaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.46(09) [September 2017]

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