Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia

The effect of the sea level rise has been detected globally, this study taken more seriously due to the existence of phenomenon such as sea water intrusion, increase of sea waves and coastal erosion. The objective of this study is to determine fluctuation of high and low tides of the South China Se...

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Main Authors: Muhammad Barzani, Gasim, Mohd Khairul Amri, Kamarudin, Hafizah, Juahir, Azman, Azid, Azizah, Endut
Format: Conference or Workshop Item
Language:English
Published: 2016
Subjects:
Online Access:http://eprints.unisza.edu.my/779/1/FH03-ESERI-17-09075.pdf
http://eprints.unisza.edu.my/779/
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spelling my-unisza-ir.7792020-10-27T06:29:32Z http://eprints.unisza.edu.my/779/ Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia Muhammad Barzani, Gasim Mohd Khairul Amri, Kamarudin Hafizah, Juahir Azman, Azid Azizah, Endut Q Science (General) TA Engineering (General). Civil engineering (General) The effect of the sea level rise has been detected globally, this study taken more seriously due to the existence of phenomenon such as sea water intrusion, increase of sea waves and coastal erosion. The objective of this study is to determine fluctuation of high and low tides of the South China Sea based on change on water quality trend of Marang and Paka Rivers and from a well monitoring in Terengganu. Sampling was done twice, first in November 2012 and was repeated in November 2015. Selected water quality parameters such as salinity, EC, TDS, DO, pH and turbidity were measured using standard instruments, nine parameters from monitoring well such as Ca, Na, Mg, Fe, Cl, TDS, TSS, EC and pH were carried out from 2006 to 2012. Two-way t-test was used for statistical analysis in this study. There is significant temporal variation in DO and turbidity meanwhile for pH, significant variation is only present during low tide in Marang River. These parameters show an increasing trend from downstream to upstream between 2012 and 2015 due to the increase of land use activities, while other parameters such as EC, salinity, TDS as well as pH were decreased during high tide in Marang River and high and low tides in Paka River. These results were concluded that global change coupled with the enactment of heavy storm and flood phenomenon during 2014 and other external causes was lead to the rising of sea level and salinity dilution of the South China Sea. 2016 Conference or Workshop Item NonPeerReviewed text en http://eprints.unisza.edu.my/779/1/FH03-ESERI-17-09075.pdf Muhammad Barzani, Gasim and Mohd Khairul Amri, Kamarudin and Hafizah, Juahir and Azman, Azid and Azizah, Endut (2016) Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia. In: Second International Conference on Science, Engineering & Environment, 21- 23 Nov 2016, Osaka, Japan.
institution Universiti Sultan Zainal Abidin
building UNISZA Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Sultan Zainal Abidin
content_source UNISZA Institutional Repository
url_provider https://eprints.unisza.edu.my/
language English
topic Q Science (General)
TA Engineering (General). Civil engineering (General)
spellingShingle Q Science (General)
TA Engineering (General). Civil engineering (General)
Muhammad Barzani, Gasim
Mohd Khairul Amri, Kamarudin
Hafizah, Juahir
Azman, Azid
Azizah, Endut
Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
description The effect of the sea level rise has been detected globally, this study taken more seriously due to the existence of phenomenon such as sea water intrusion, increase of sea waves and coastal erosion. The objective of this study is to determine fluctuation of high and low tides of the South China Sea based on change on water quality trend of Marang and Paka Rivers and from a well monitoring in Terengganu. Sampling was done twice, first in November 2012 and was repeated in November 2015. Selected water quality parameters such as salinity, EC, TDS, DO, pH and turbidity were measured using standard instruments, nine parameters from monitoring well such as Ca, Na, Mg, Fe, Cl, TDS, TSS, EC and pH were carried out from 2006 to 2012. Two-way t-test was used for statistical analysis in this study. There is significant temporal variation in DO and turbidity meanwhile for pH, significant variation is only present during low tide in Marang River. These parameters show an increasing trend from downstream to upstream between 2012 and 2015 due to the increase of land use activities, while other parameters such as EC, salinity, TDS as well as pH were decreased during high tide in Marang River and high and low tides in Paka River. These results were concluded that global change coupled with the enactment of heavy storm and flood phenomenon during 2014 and other external causes was lead to the rising of sea level and salinity dilution of the South China Sea.
format Conference or Workshop Item
author Muhammad Barzani, Gasim
Mohd Khairul Amri, Kamarudin
Hafizah, Juahir
Azman, Azid
Azizah, Endut
author_facet Muhammad Barzani, Gasim
Mohd Khairul Amri, Kamarudin
Hafizah, Juahir
Azman, Azid
Azizah, Endut
author_sort Muhammad Barzani, Gasim
title Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
title_short Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
title_full Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
title_fullStr Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
title_full_unstemmed Is the South China Sea has undergone a sea level rise? A preliminary study in Terengganu, Malaysia
title_sort is the south china sea has undergone a sea level rise? a preliminary study in terengganu, malaysia
publishDate 2016
url http://eprints.unisza.edu.my/779/1/FH03-ESERI-17-09075.pdf
http://eprints.unisza.edu.my/779/
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