COASTAL UPWELLING IN THE VICINITY OF TIOMAN ISLAND

dc.contributor.authorZURAINI ZAINOL
dc.contributor.authorMOHD FADZIL AKHIR
dc.date.accessioned2017-10-04T03:42:36Z
dc.date.available2017-10-04T03:42:36Z
dc.date.issued2016
dc.description.abstractThe coastal upwelling in Tioman Island vicinity was studied using the Conductivity, Temperature, Depth sensor (CTD) and Acoustic Doppler Current Profier (ADCP) data collection and model output during June and August 2014. Different coastal upwelling strength was noted around the island, where the temperature records during the study was on average 0.6 °C cooler at the north (3.1°N latitude) than the south (2.6°N latitude) parts. Slightly high magnitude of increased current speed (~60 cm/s) at the north part of Tioman Island was believed to be the causative factor of the observed temperature difference. Analysis on the vertical section of density and northsouth velocity confimed the separation of current speed in the water column around the island, meanwhile the model simulation of the current circulation during August, 2014 proved the presence of increase current with an average speed of 0.34 m/s around Tioman Island especially at the north of the island.en_US
dc.identifier.issn1823 8556
dc.identifier.urihttp://hdl.handle.net/123456789/6951
dc.language.isoenen_US
dc.publisherThe International Seminar on the Straits of Malacca and the South China Sea 2016en_US
dc.subjectCoastal upwellingen_US
dc.subjecttemperatureen_US
dc.subjectcurrentsen_US
dc.subjectwind stressen_US
dc.subjectTioman Islanden_US
dc.subjectSouth China Seaen_US
dc.titleCOASTAL UPWELLING IN THE VICINITY OF TIOMAN ISLANDen_US
dc.typeArticleen_US
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