Sediment variation along the east coast of Peninsular Malaysia

• Autorzy: MatAmin A.R. , Ahmad F. , Mamat M. , Rivaie M. , Abdullah K.
• Języki publikacji: EN

Abstrakty

EN

The northeast monsoon season (NEMS), which occurs between November and March every year, brings heavy rains and strong wind to the east coast of Peninsular Malaysia. Large sediment resuspension during this season is caused by high waves and river discharge carried by the river to the sea. Sediment is defined in this research as both organic and inorganic materials. Remote sensing reflectance (Rrs) of the Moderate Resolution Spectroradiometer (MODIS) 667 nm channel is used in this study as a Total Suspended Sediment (TSS) index. The data was acquired from Aqua satellite with 9 km resolution. The study was conducted along the eastern coast of Peninsular Malaysia over the period of 2002-2012. The result shows that TSS along the Peninsular Malaysia coastline and the river mouth is highly seasonal. The highest TSS is observed during NEMS with the peak value in November-December every year.

• Wydawca: -
• Czasopismo: Ecological Questions
• Rocznik: 2012
• Tom: 16
• Opis fizyczny: p.99-108,fig.,ref.

Twórcy

autor

MatAmin A.R.

• Faculty of Maritime Studies and Marine Science, Universiti Malaysia Terengganu, 21030 Kuala Terengganu, Terengganu, Malaysia
• Faculty of Applied Science, Universiti Teknologi MARA Terengganu, Kampus Kuala Terengganu, 21080 Kuala Terengganu, Terengganu, Malaysia

autor

Ahmad F.

• Faculty of Maritime Studies and Marine Science, Universiti Malaysia Terengganu, 21030 Kuala Terengganu, Terengganu, Malaysia

autor

Mamat M.

• Fakulti Informatik dan Komputeran, Universiti Sultan Zainal Abidin, Kampus Tembila, 22200 Besut, Terengganu, Malaysia

autor

Rivaie M.

• Faculty of Maritime Studies and Marine Science, Universiti Malaysia Terengganu, 21030 Kuala Terengganu, Terengganu, Malaysia

autor

Abdullah K.

• School of Physics, Universiti Sains Malaysia, 11800 Minden, Malaysia

Bibliografia

• Acker J.G. & Leptoukh G., 2007, Online Analysis Enhances Use of NASA Earth Science Data, Eos, Transactions of American Geophyscs Union 88(2): 14 and 17.
• Global Environment (SAGE) website [http://www.sage.wisc.edu/riverdata].
• Hussain M. L., Yaakob R., & Saad S., 1995, Beach erosion variability during a Northeast Monsoon: The Kuala Setiu Coastline, Terengganu, Malaysia, Pertanika Journal of Science and Technology 3(2): 337-348.
• Kuang R., Zhou Y. & Zhu Y., 2011, Monitoring transport of suspended sediment in the Nanhui nearshore integrating remote sensing images with hydrodynamic model, [in:] Geoinformatics’ 2011, 19th International Conference on IEEE: 1-4.
• Malaysia Meteorology Department, Weather Phenomenon website [http://www.met.gov.my], [accessed 09.2012].
• May C.L., Koseff J.R., Lucas L.V., Cloern J.E. & Schoellhamer D.H., 2003, Effects of spatial and temporal var- iability of turbidity on phytoplankton blooms, Marine Ecology Progress Ser. 25: 111-128.
• Mayer L.M., Keil R.G., Macko S.A., Joye S.B., Ruttenberg K.C. & Aller R.C., 1998, Importance of suspended participates in riverine delivery of bioavailable nitrogen to coastal zones, Global Biogeochemical Cycles, 12: 573-579.
• Miller R.L. & Cruise J.F., 1995, Effects of suspended sediments on coral growth: Evidence from remote sensing and hydrologic modeling, Remote Sensing of Environment 53: 177-187.[http://dx.doi.org/10.1016/0034-4257(95)00081-B]
• Miller R.L. & McKee B.A., 2004, Using MODIS Terra 250 m imagery to map concentrations of total suspended matter in coastal waters, Remote Sensing of Environment 93: 259-266.
• Min J.E., Ryu J.H., Lee S. & Son S., 2012, Monitoring of suspended sediment variation using Landsat and MODIS in the Saemangeum coastal area of Korea, Marine Pollution Bulletin 64: 382-390.[http://www.ncbi.nlm.nih.gov/pubmed/22136763] [http://dx.doi.org/10.1016/j.marpolbul.2011.10.025]
• National Aeronautics and Space Administration website [http://gdata1.sci.gsfc.nasa.gov/daac-bin/G3/gui.cgi?instance_id=ocean_month].
• Olsen C.F., Cutshall N.H. & Larsen I.L., 1982, Pollutant- particle associations and dynamics in coastal marine environments: a review, Marine Chemistry 11: 501-533.[http://dx.doi.org/10.1016/0304-4203(82)90001-9]
• Pavelsky T.M. & Smith L.C., 2009, Remote sensing of suspended sediment concentration, flow velocity, and lake recharge in the Peace-Althabasca Delta, Canada, Water Resources Research 45: W11417.
• Prasad A.K. & Singh R.P., 2010, Chlorophyll, calcite, and suspended sediment concentrations in the Bay of Bengal and the Arabian Sea at the river mouths, Advances in Space Research 45: 61-69.
• RSS WindSat [available at www.remss.com].
• Schallenberg M. & Burns C.W., 2004, Effects of sediment resuspension on phytoplankton production: teasing apart the influences of light, nutrients and algal entrainment, Freshwater Biology 49(2): 143-159.[http://dx.doi.org/10.1046/j.1365-2426.2003.01172.x]
• Salomonson V.V., Barnes W.L., Maymon P.W., Montgomery H.E. & Ostrow H., 1989, MODIS: Advanced facility instrument for studies of the Earth as a system, IEEE Transactions on Geoscience and Remote Sensing 27: 145-153.[http://dx.doi.org/10.1109/36.20292]
• Villar E.R., Martinez J.M., Le Texier M., Guyot J.L., Fraizy P., Meneses P.R. & Oliveira E.D., 2012, A study of sediment transport in the Madeira River, Brazil, using MODIS remote-sensing images, Journal of South American Earth Sciences (2012), [doi: 10.1016/j. jsames], [accessed 06.11.2012].[http://dx.doi.org/10.1016/j.jsames],[accessed06.11.2012]]
• Wang J.J. & Lu X.X., 2010, Estimation of suspended sediment concentrations using Terra MODIS: An example from the Lower Yangtze River, China Sciience of the Total Environment 408(5): 1131-1138. [http://www.ncbi.nlm.nih.gov/pubmed/20022078]

Identyfikatory

DOI

10.2478/v10090-012-0010-6