Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data

This study was conducted to investigate the temporal and spatial variation of the chlorophyll-a concentration over the past 13 years of Sea-viewing Wide Field-of-view Sensor (SeaWiFS) mission in the Sulu Sea area. The objectives of this study are to analyze the long term and spatial variability of t...

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Main Authors: Abd. Latiff, Nurzuliana Atiqah Aainaa, Md. Reba, Mohd. Nadzri, Siswanto, Eko
Format: Article
Language:English
Published: Institute of Physics Publishing 2014
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Online Access:http://eprints.utm.my/id/eprint/52349/1/NurzulianaAtiqahAainaa2014_Determiningtemporalandspatial.pdf
http://eprints.utm.my/id/eprint/52349/
http://dx.doi.org/10.1088/1755-1315/18/1/012114
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spelling my.utm.523492018-09-17T04:08:07Z http://eprints.utm.my/id/eprint/52349/ Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data Abd. Latiff, Nurzuliana Atiqah Aainaa Md. Reba, Mohd. Nadzri Siswanto, Eko HD Industries. Land use. Labor This study was conducted to investigate the temporal and spatial variation of the chlorophyll-a concentration over the past 13 years of Sea-viewing Wide Field-of-view Sensor (SeaWiFS) mission in the Sulu Sea area. The objectives of this study are to analyze the long term and spatial variability of the Chl-a concentration in Sulu Sea with special emphasize on the relationship between Chl-a concentration with the other oceanographic parameters such as sea surface temperature (SST), wind speed and wind directions. The Chl-a concentration were high during northeast monsoon which experience low SST. The fluctuation of Chl-a and SST are associated by the wind speed variation in this area. This suggests that during northeast monsoon, the increasing of wind speed intensifies water column mixing which entrains submerged cold- and nutrient-rich deep water to the surface layer, resulting in low SST and high nutrient in the surface layer. On the other hand, the southwest monsoon records dramatically decreasing of the Chl-a with regard to lower wind speed and surface water heating occurance. This promotes the downwelling process and weakens the upwelling one in the Sulu Sea [1] and as a result, this phenomenon influence reduction of nutrient upwelling to the surface layer, and thus produces lower Chl-a throughout the seasonal periods Institute of Physics Publishing 2014 Article PeerReviewed application/pdf en http://eprints.utm.my/id/eprint/52349/1/NurzulianaAtiqahAainaa2014_Determiningtemporalandspatial.pdf Abd. Latiff, Nurzuliana Atiqah Aainaa and Md. Reba, Mohd. Nadzri and Siswanto, Eko (2014) Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data. 8th International Symposium of the Digital Earth (ISDE8), 18 (1). ISSN 1755-1315 http://dx.doi.org/10.1088/1755-1315/18/1/012114 DOI: 10.1088/1755-1315/18/1/012114
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
language English
topic HD Industries. Land use. Labor
spellingShingle HD Industries. Land use. Labor
Abd. Latiff, Nurzuliana Atiqah Aainaa
Md. Reba, Mohd. Nadzri
Siswanto, Eko
Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
description This study was conducted to investigate the temporal and spatial variation of the chlorophyll-a concentration over the past 13 years of Sea-viewing Wide Field-of-view Sensor (SeaWiFS) mission in the Sulu Sea area. The objectives of this study are to analyze the long term and spatial variability of the Chl-a concentration in Sulu Sea with special emphasize on the relationship between Chl-a concentration with the other oceanographic parameters such as sea surface temperature (SST), wind speed and wind directions. The Chl-a concentration were high during northeast monsoon which experience low SST. The fluctuation of Chl-a and SST are associated by the wind speed variation in this area. This suggests that during northeast monsoon, the increasing of wind speed intensifies water column mixing which entrains submerged cold- and nutrient-rich deep water to the surface layer, resulting in low SST and high nutrient in the surface layer. On the other hand, the southwest monsoon records dramatically decreasing of the Chl-a with regard to lower wind speed and surface water heating occurance. This promotes the downwelling process and weakens the upwelling one in the Sulu Sea [1] and as a result, this phenomenon influence reduction of nutrient upwelling to the surface layer, and thus produces lower Chl-a throughout the seasonal periods
format Article
author Abd. Latiff, Nurzuliana Atiqah Aainaa
Md. Reba, Mohd. Nadzri
Siswanto, Eko
author_facet Abd. Latiff, Nurzuliana Atiqah Aainaa
Md. Reba, Mohd. Nadzri
Siswanto, Eko
author_sort Abd. Latiff, Nurzuliana Atiqah Aainaa
title Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
title_short Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
title_full Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
title_fullStr Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
title_full_unstemmed Determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
title_sort determining temporal and spatial variabilities of biological production in sulu sea using multi-remotely sensed data
publisher Institute of Physics Publishing
publishDate 2014
url http://eprints.utm.my/id/eprint/52349/1/NurzulianaAtiqahAainaa2014_Determiningtemporalandspatial.pdf
http://eprints.utm.my/id/eprint/52349/
http://dx.doi.org/10.1088/1755-1315/18/1/012114
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score 13.211869