Sediment dynamics at Puri and Konark beaches, along northeast coast of India
The influence of annual and long term variations in the prevalent environmental conditions along the coast of Orissa, India between 1978-1985 (beach profile measurement between 1979-1982) has been evaluated. The results suggest that during December-February, southerly drift nourishes the beaches, an...
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| Veröffentlicht in: | Indian journal of marine sciences 1992-09, Vol.21 (3), p.201-206 |
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| container_title | Indian journal of marine sciences |
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| creator | CHAUHAN, O. S |
| description | The influence of annual and long term variations in the prevalent environmental conditions along the coast of Orissa, India between 1978-1985 (beach profile measurement between 1979-1982) has been evaluated. The results suggest that during December-February, southerly drift nourishes the beaches, and during May-September, waves with high energy density, unfavorably wave steepness and littoral currents from southwest induce erosion. Between 1979-82, the Konark Coast had an accretionary tendency owing to the favorable location of the area with respect to a fluvial source. The Puri Coast however, had an erosional tendency. About 5.37 m super(3).m/ly/l sediments were eroded between 1979-82 from this portion of the coast. This is in addition to the erosion induced by a moderate cyclone/depression, which on an average eroded about 70 m super(3).m/l sediments per cyclone. |
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S</creator><creatorcontrib>CHAUHAN, O. S</creatorcontrib><description>The influence of annual and long term variations in the prevalent environmental conditions along the coast of Orissa, India between 1978-1985 (beach profile measurement between 1979-1982) has been evaluated. The results suggest that during December-February, southerly drift nourishes the beaches, and during May-September, waves with high energy density, unfavorably wave steepness and littoral currents from southwest induce erosion. Between 1979-82, the Konark Coast had an accretionary tendency owing to the favorable location of the area with respect to a fluvial source. The Puri Coast however, had an erosional tendency. About 5.37 m super(3).m/ly/l sediments were eroded between 1979-82 from this portion of the coast. This is in addition to the erosion induced by a moderate cyclone/depression, which on an average eroded about 70 m super(3).m/l sediments per cyclone.</description><identifier>ISSN: 0379-5136</identifier><identifier>EISSN: 0975-1033</identifier><identifier>CODEN: IJMNBF</identifier><language>eng</language><publisher>New Delhi: Council of Scientific & Industrial Research</publisher><subject>Coastal oceanography, estuaries. 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Regional oceanography</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Marine</topic><topic>Marine and continental quaternary</topic><topic>Physics of the oceans</topic><topic>Surficial geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>CHAUHAN, O. S</creatorcontrib><collection>Pascal-Francis</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Indian journal of marine sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>CHAUHAN, O. S</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sediment dynamics at Puri and Konark beaches, along northeast coast of India</atitle><jtitle>Indian journal of marine sciences</jtitle><date>1992-09-01</date><risdate>1992</risdate><volume>21</volume><issue>3</issue><spage>201</spage><epage>206</epage><pages>201-206</pages><issn>0379-5136</issn><eissn>0975-1033</eissn><coden>IJMNBF</coden><abstract>The influence of annual and long term variations in the prevalent environmental conditions along the coast of Orissa, India between 1978-1985 (beach profile measurement between 1979-1982) has been evaluated. The results suggest that during December-February, southerly drift nourishes the beaches, and during May-September, waves with high energy density, unfavorably wave steepness and littoral currents from southwest induce erosion. Between 1979-82, the Konark Coast had an accretionary tendency owing to the favorable location of the area with respect to a fluvial source. The Puri Coast however, had an erosional tendency. About 5.37 m super(3).m/ly/l sediments were eroded between 1979-82 from this portion of the coast. This is in addition to the erosion induced by a moderate cyclone/depression, which on an average eroded about 70 m super(3).m/l sediments per cyclone.</abstract><cop>New Delhi</cop><pub>Council of Scientific & Industrial Research</pub><tpages>6</tpages></addata></record> |
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| ispartof | Indian journal of marine sciences, 1992-09, Vol.21 (3), p.201-206 |
| issn | 0379-5136 0975-1033 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_16386535 |
| source | Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Coastal oceanography, estuaries. Regional oceanography Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Marine Marine and continental quaternary Physics of the oceans Surficial geology |
| title | Sediment dynamics at Puri and Konark beaches, along northeast coast of India |
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