Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park

Remote sensing is one of the important tools used to measure sea surface temperature (SST). The main purpose of this study is to determine sea temperature in Talang Satang National Park (TSNP) and to relate it with El Niño Southern Oscillation (ENSO). Sea temperature in TSNP is measured using HOBO...

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Main Author: Nur Asilah, binti Awang
Format: Final Year Project Report
Language:English
Published: Universiti Malaysia Sarawak, (UNIMAS) 2014
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Online Access:http://ir.unimas.my/id/eprint/8277/1/Asilah.pdf
http://ir.unimas.my/id/eprint/8277/
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spelling my.unimas.ir.82772023-06-21T03:38:16Z http://ir.unimas.my/id/eprint/8277/ Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park Nur Asilah, binti Awang GE Environmental Sciences Remote sensing is one of the important tools used to measure sea surface temperature (SST). The main purpose of this study is to determine sea temperature in Talang Satang National Park (TSNP) and to relate it with El Niño Southern Oscillation (ENSO). Sea temperature in TSNP is measured using HOBO Light/Temperature Data Logger and AVHRR satellite sensor. The mean sea temperature from data logger is 30.14 ± 0.74 ºC, while the sea temperature from the satellite is 29.52 ± 0.71 ºC. The reliability of SST retrieved from the satellite in TSNP is questioned. Consecutively, the satellite datasets for SST in TSNP is compared with data logger. There is high correlation between these two instruments (r = 0.792). Satellite managed to record the trends of SST, but not providing the absolute value. From the recorded trends, it shows TSNP is influenced by seasonal monsoon; namely the Northeast (NE) monsoon (November - March) and Southwest (SW) monsoon (May – September). Monsoon caused the variability of SST. High SST recorded during SW monsoon and the transitional months, but low SST during the NE monsoon. There were double maximum peak of SST every year; highest in June, followed by October. The SST in the year 2008 to 2011 were significantly different than others due to strong ENSO event. Strong ENSO event gives impact to SW monsoon, which causes significant difference (p < 0.05) in SST during these periods. Forecasting ENSO event is possible only by several months ahead. SST anomalies from previous strong El Niño episode (2009) are compared with the prediction of El Niño (summer 2014). High correlation (r = 0.614) between these anomalies indicates the incoming El Niño may affect the SST in TSNP. Universiti Malaysia Sarawak, (UNIMAS) 2014 Final Year Project Report NonPeerReviewed text en http://ir.unimas.my/id/eprint/8277/1/Asilah.pdf Nur Asilah, binti Awang (2014) Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park. [Final Year Project Report] (Unpublished)
institution Universiti Malaysia Sarawak
building Centre for Academic Information Services (CAIS)
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Sarawak
content_source UNIMAS Institutional Repository
url_provider http://ir.unimas.my/
language English
topic GE Environmental Sciences
spellingShingle GE Environmental Sciences
Nur Asilah, binti Awang
Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
description Remote sensing is one of the important tools used to measure sea surface temperature (SST). The main purpose of this study is to determine sea temperature in Talang Satang National Park (TSNP) and to relate it with El Niño Southern Oscillation (ENSO). Sea temperature in TSNP is measured using HOBO Light/Temperature Data Logger and AVHRR satellite sensor. The mean sea temperature from data logger is 30.14 ± 0.74 ºC, while the sea temperature from the satellite is 29.52 ± 0.71 ºC. The reliability of SST retrieved from the satellite in TSNP is questioned. Consecutively, the satellite datasets for SST in TSNP is compared with data logger. There is high correlation between these two instruments (r = 0.792). Satellite managed to record the trends of SST, but not providing the absolute value. From the recorded trends, it shows TSNP is influenced by seasonal monsoon; namely the Northeast (NE) monsoon (November - March) and Southwest (SW) monsoon (May – September). Monsoon caused the variability of SST. High SST recorded during SW monsoon and the transitional months, but low SST during the NE monsoon. There were double maximum peak of SST every year; highest in June, followed by October. The SST in the year 2008 to 2011 were significantly different than others due to strong ENSO event. Strong ENSO event gives impact to SW monsoon, which causes significant difference (p < 0.05) in SST during these periods. Forecasting ENSO event is possible only by several months ahead. SST anomalies from previous strong El Niño episode (2009) are compared with the prediction of El Niño (summer 2014). High correlation (r = 0.614) between these anomalies indicates the incoming El Niño may affect the SST in TSNP.
format Final Year Project Report
author Nur Asilah, binti Awang
author_facet Nur Asilah, binti Awang
author_sort Nur Asilah, binti Awang
title Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
title_short Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
title_full Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
title_fullStr Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
title_full_unstemmed Satellite and In-Situ Measurement for Temporal Variability of Sea Temperature in Talang Satang National Park
title_sort satellite and in-situ measurement for temporal variability of sea temperature in talang satang national park
publisher Universiti Malaysia Sarawak, (UNIMAS)
publishDate 2014
url http://ir.unimas.my/id/eprint/8277/1/Asilah.pdf
http://ir.unimas.my/id/eprint/8277/
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score 13.211869