Sains Malaysiana 46(8)(2017): 1191–1200
http://dx.doi.org/10.17576/jsm-2017-4608-04
Factors Influencing
the Distribution of Chl-a along Coastal
Waters of East Peninsular Malaysia
(Faktor Mempengaruhi Taburan Chl-a di Pesisir Pantai Timur Semenanjung Malaysia)
F. SHAARI
& M.A. MUSTAPHA*
School of Environmental
and Natural Resource Sciences, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600
UKM Bangi, Selangor Darul Ehsan, Malaysia
Diserahkan: 14 Jun 2016/Diterima: 8 Februari 2017
ABSTRACT
Determination of
chlorophyll-a (Chl-a) distribution in the coastal
waters is important to understand the coastal environmental conditions. This
study was conducted to understand the spatial and temporal distribution of Chl-a along coastal waters of east Peninsular Malaysia and
factors influencing its variability using Chl-a data
derived from Aqua MODIS satellite (1 km spatial
resolution) from January 2006 to December 2012. Chl-a variability was described using empirical orthogonal
function (EOF) analysis. In-situ data (temperature, salinity, density and nitrate) and rainfall data from the
Department of Meteorology were analyzed using spatial interpolation to
determine factors influencing the distribution of Chl-a. The seasonal progressions of Chl-a
showed high value during northeast monsoon along the coast. This
variability was described by four modes of the EOF analysis.
The first mode (72.08% of total variance) indicated seasonal cycle with high
variability along the coast. Second mode (17.03% of variance) explained the
northeast monsoon with high variability from river mouth to the south. Third
mode (2.39% of variance) indicated variability during southwest monsoon along
the coast and much higher to the south. Mode 4 (1.93% of variance) explained
the inter-monsoon period observed along the northern and southern coastline.
Concentration and distribution of Chl-a were related to availability of nutrient influenced by
rainfall. The thermohaline front was also observed to play an important role in
accumulation of phytoplankton biomass during northeast and southwest monsoon.
Keywords: Chl-a; Coastal waters; empirical orthogonal function (EOF);
nitrate
ABSTRAK
Penentuan taburan klorofil-a
(Chl-a) di pesisir
pantai adalah penting
bagi memahami
keadaan persekitaran pesisir pantai. Penyelidikan ini
telah dijalankan
untuk memahami taburan reruang dan masa Chl-a di pesisiran pantai timur Semenanjung Malaysia dan faktor yang mempengaruhi variasi taburan menggunakan data Chl-a daripada satelit Aqua MODIS (1 km resolusi
reruang) dari
Januari 2006 hingga Disember 2012. Variasi Chl-a diterangkan
dengan mengunakan
analisis fungsi ortogon empirik (EOF).
Data in-situ
(suhu, saliniti, ketumpatan dan nitrat) serta data hujan daripada Jabatan
Meteorologi dianalisis
dengan menggunakan interpolasi reruang bagi menentukan faktor yang mempengaruhi taburan Chl-a. Taburan musiman Chl-a menunjukkan
kepekatan tertinggi
semasa monsun timur
laut dan
tersebar di sepanjang pesisir pantai. Variasi ini diterangkan melalui empat mod analisis EOF. Mod
pertama (72.08% daripada
jumlah varians) menerangkan kitaran bermusim dengan variasi yang tinggi sepanjang pesisir pantai. Mod kedua
(17.03% daripada jumlah
varians) menerangkan keadaan monsun timur laut dengan
variasi yang tinggi
di muara sungai ke
arah selatan.
Mod ketiga (2.39% varians)
menunjukkan keadaan
monsun barat daya
di sepanjang pesisir
pantai dan lebih
tinggi di bahagian
selatan. Mod keempat
(1.93% variasi) pula menerangkan
keadaan peralihan
iaitu di sepanjang bahagian utara dan selatan pesisir
pantai. Kepekatan dan taburan
klorofil-a di bahagian selatan pesisir pantai didapati berhubungan dengan ketersediaan nutrien yang dipengaruhi oleh curahan hujan. Struktur
termohalin didapati memainkan peranan yang penting terhadap pengumpulan biojisim fitoplankton semasa monsun timur laut
dan barat
daya.
Kata kunci: Chl-a; fungsi ortogon empirik (EOF); nitrat; pesisir pantai
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*Pengarang untuk surat-menyurat; email: muzz@ukm.edu.my