Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf

The Arabian Gulf is a highly turbid, shallow sedimentary basin whose coastal areas have been classified as optically complex Case II waters (where ocean colour sensors have been proved to be unreliable). Yet, there is no such study assessing the performance and quality of satellite ocean-colour data...

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Main Authors: Noora Al-Naimi, Dionysios E. Raitsos, Radhouan Ben-Hamadou, Yousria Soliman
Format: Article
Language:English
Published: MDPI AG 2017-03-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/9/3/301
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author Noora Al-Naimi
Dionysios E. Raitsos
Radhouan Ben-Hamadou
Yousria Soliman
author_facet Noora Al-Naimi
Dionysios E. Raitsos
Radhouan Ben-Hamadou
Yousria Soliman
author_sort Noora Al-Naimi
collection DOAJ
description The Arabian Gulf is a highly turbid, shallow sedimentary basin whose coastal areas have been classified as optically complex Case II waters (where ocean colour sensors have been proved to be unreliable). Yet, there is no such study assessing the performance and quality of satellite ocean-colour datasets in relation to ground truth data in the Gulf. Here, using a unique set of in situ Chlorophyll-a measurements (Chl-a; an index of phytoplankton biomass), collected from 24 locations in four transects in the central Gulf over six recent research cruises (2015–2016), we evaluated the performance of VIIRS and other merged satellite datasets, for the first time in the region. A highly significant relationship was found (r = 0.795, p < 0.001), though a clear overestimation in satellite-derived Chl-a concentrations is evident. Regardless of this constant overestimation, the remotely sensed Chl-a observations illustrated adequately the seasonal cycles. Due to the optically complex environment, the first optical depth was calculated to be on average 6–10 m depth, and thus the satellite signal is not capturing the deep chlorophyll maximum (DCM at ~25 m). Overall, the ocean colour sensors’ performance was comparable to other Case II waters in other regions, supporting the use of satellite ocean colour in the Gulf. Yet, the development of a regional-tuned algorithm is needed to account for the unique environmental conditions of the Gulf, and ultimately provide a better estimation of surface Chl-a in the region.
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spelling doaj.art-43a482d9552d46c488436ae755467bb02022-12-21T19:25:42ZengMDPI AGRemote Sensing2072-42922017-03-019330110.3390/rs9030301rs9030301Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian GulfNoora Al-Naimi0Dionysios E. Raitsos1Radhouan Ben-Hamadou2Yousria Soliman3Environmental Science Center (ESC), Qatar University (QU), P.O. Box 2317, Doha, QatarPlymouth Marine Laboratory (PML), Prospect Place, The Hoe, Plymouth PL1 3DH, UKDepartment of Biological and Environmental Science, Qatar University (QU), P.O. Box 2317, Doha, QatarDepartment of Biological and Environmental Science, Qatar University (QU), P.O. Box 2317, Doha, QatarThe Arabian Gulf is a highly turbid, shallow sedimentary basin whose coastal areas have been classified as optically complex Case II waters (where ocean colour sensors have been proved to be unreliable). Yet, there is no such study assessing the performance and quality of satellite ocean-colour datasets in relation to ground truth data in the Gulf. Here, using a unique set of in situ Chlorophyll-a measurements (Chl-a; an index of phytoplankton biomass), collected from 24 locations in four transects in the central Gulf over six recent research cruises (2015–2016), we evaluated the performance of VIIRS and other merged satellite datasets, for the first time in the region. A highly significant relationship was found (r = 0.795, p < 0.001), though a clear overestimation in satellite-derived Chl-a concentrations is evident. Regardless of this constant overestimation, the remotely sensed Chl-a observations illustrated adequately the seasonal cycles. Due to the optically complex environment, the first optical depth was calculated to be on average 6–10 m depth, and thus the satellite signal is not capturing the deep chlorophyll maximum (DCM at ~25 m). Overall, the ocean colour sensors’ performance was comparable to other Case II waters in other regions, supporting the use of satellite ocean colour in the Gulf. Yet, the development of a regional-tuned algorithm is needed to account for the unique environmental conditions of the Gulf, and ultimately provide a better estimation of surface Chl-a in the region.http://www.mdpi.com/2072-4292/9/3/301Arabian GulfphytoplanktonChlorophyll-aocean colourremote sensingOC-CCI
spellingShingle Noora Al-Naimi
Dionysios E. Raitsos
Radhouan Ben-Hamadou
Yousria Soliman
Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
Remote Sensing
Arabian Gulf
phytoplankton
Chlorophyll-a
ocean colour
remote sensing
OC-CCI
title Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
title_full Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
title_fullStr Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
title_full_unstemmed Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
title_short Evaluation of Satellite Retrievals of Chlorophyll-a in the Arabian Gulf
title_sort evaluation of satellite retrievals of chlorophyll a in the arabian gulf
topic Arabian Gulf
phytoplankton
Chlorophyll-a
ocean colour
remote sensing
OC-CCI
url http://www.mdpi.com/2072-4292/9/3/301
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