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Water mass properties, variabilities and origins in northern bornea

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dc.contributor.author Shukri Arsad
dc.date.accessioned 2015-06-13T08:00:48Z
dc.date.available 2015-06-13T08:00:48Z
dc.date.issued 2013-12
dc.identifier.uri http://hdl.handle.net/123456789/3417
dc.description.abstract We present a definition of water mass properties, variabilities and origins along the coast of northern Borneo based on 55 CTD casts taken during cruises in July 2009. We also studied data from four Argo profiling floats in the surrounding seas. The temperature salinity (TS) relation in the South China Sea, Sulu Sea and Celebes Sea show the existence of eight water masses. Earlier studies defined the surface mixed layer water masses as Open Sea Water (OSW), Continental Shelf Water (CSW) and Seasonal Thermocline Water (STW). Below the layer of this active mixing are subsurface zones of rapid transition called the Tropical Surface Water (TSW) and Maximum Salinity Water (MaxSW). Permanent Thermocline Water (PTW), Minimum Salinity Water (MinSW) and Deep Water (DW) are at the intermediate layer to about 1000 m. en_US
dc.language.iso en en_US
dc.publisher Terengganu: Universiti Malaysia Terengganu en_US
dc.subject GC 300 .S5 2013 en_US
dc.subject Shukri Arsad en_US
dc.subject Thesis INOS 2013 en_US
dc.subject Water masses en_US
dc.title Water mass properties, variabilities and origins in northern bornea en_US
dc.type Thesis en_US


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