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The geographical influence towards current circulation and physical characteristics of Bidong Island

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dc.contributor.author Nur Afiqah Samat
dc.date.accessioned 2018-11-21T03:08:46Z
dc.date.available 2018-11-21T03:08:46Z
dc.date.issued 2012
dc.identifier.uri http://umt-ir.umt.edu.my:8080/xmlui/handle/123456789/10172
dc.description.abstract This study was conducted to analyze and determine current circulation pattern and physical characteristics ofBidong Island water from data collected on June 2011. The insitu data was collected by using Hydrolab Quanta and Acoustic Doppler Current Profiler (ADCP). The data was analyzed by using MATLAB software and Microsoft Excel. The data were grouped into Group A, Group B, Group C and Group D in order to determine the geographical influence towards current circulation pattern, temperature and salinity. From the result obtained, temperature values were from 25.56 to 29.84 °C. Group B recorded lower temperature while temperature distributions of Group D were highest. Salinity in Bidong Island was from 32.49 to 33.52 ppt. Distributions of salinity were almost constant except for Group B. Results showed stratification layer at Bidong Island. Current circulation profile was almost constant in directions and speeds from surface to 5 m. Currents move in mix direction, suspected to be result of deflection and recirculation. Most of currents were directed to northwest and southwest. Currents at upper side of Bidong Island which was Group A and Group C were more consistent in direction than Group B and Group D. Inconsistent of current circulation area were surrounded near Karah Island in which below Bidong Island. It is suspected that there is geographical influenced between the islands. en_US
dc.language.iso en en_US
dc.publisher Terengganu: Universiti Malaysia Terengganu en_US
dc.subject LP 30 FMSM 3 2012 en_US
dc.subject Nur Afiqah Samat en_US
dc.title The geographical influence towards current circulation and physical characteristics of Bidong Island en_US
dc.type Working Paper en_US


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