Abstract
The Gulf of Mannar (GoM) and the Palk Bay (PB) are two least studied marine environments located between India and Sri Lanka. Exceptionally high chlorophyll a concentration in the GoM and the PB during the Northeast Monsoon (November–February) is a consistent feature in satellite imageries, which has been attributed to the intrusion of the Bay of Bengal (BoB) waters. The analyses of the Moderate Resolution Imaging Spectroradiometer (MODIS) and field chlorophyll data collected from 30 locations in the Indian sector of the GoM and the PB in January 2011 showed significant overestimations in the satellite data. This error was much higher in the PB (60–80 %) as compared to the GoM (18–28 %). The multivariate analyses evidenced that the exceptionally high satellite chlorophyll in the PB is contributed largely by turbidity, colored dissolved organic matter (CDOM), and bottom reflectance. The paper cautions that though MODIS is superior in estimating chlorophyll a in optically complex waters, there are still chances of overestimations in regions like the PB.
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Acknowledgments
The authors thank the Director, National Institute of Oceanography, India, for the facilities and encouragement. We thankfully acknowledge all our colleges in the National Institute of Oceanography, India, who helped in carrying out the seasonal fieldwork in the GoM and the PB. The authors thank the Ministry of Shipping for the financial support. This work forms a part of the Supra Institutional Project (SIP) 1302 of the National Institute of Oceanography. This is NIO contribution 5625.
The first author thankfully acknowledge Dr. Trevor Platt and Dr. Subha Sathyendranath, who taught him the far reaching applications of satellite remote sensing in oceanography.
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Jyothibabu, R., Madhu, N.V., Jagadeesan, L. et al. Why do satellite imageries show exceptionally high chlorophyll in the Gulf of Mannar and the Palk Bay during the Norteast Monsoon?. Environ Monit Assess 186, 7781–7792 (2014). https://doi.org/10.1007/s10661-014-3966-4
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DOI: https://doi.org/10.1007/s10661-014-3966-4