Retrieval of suspended sediment concentration (SSC) in the Arabian Gulf water of arid region by Sentinel-2 data

Rajendran Sankaran; Jassim A Al-Khayat; Aravinth J; Mark Edward Chatting; Fadhil N Sadooni; Hamad Al-Saad Al-Kuwari

doi:10.1016/j.scitotenv.2023.166875

Retrieval of suspended sediment concentration (SSC) in the Arabian Gulf water of arid region by Sentinel-2 data

Sci Total Environ. 2023 Dec 15:904:166875. doi: 10.1016/j.scitotenv.2023.166875. Epub 2023 Sep 6.

Authors

Rajendran Sankaran¹, Jassim A Al-Khayat², Aravinth J³, Mark Edward Chatting⁴, Fadhil N Sadooni², Hamad Al-Saad Al-Kuwari²

Affiliations

¹ Environmental Science Center, Qatar University, P.O. Box: 2713, Doha, Qatar. Electronic address: srajendran@qu.edu.qa.
² Environmental Science Center, Qatar University, P.O. Box: 2713, Doha, Qatar.
³ Department of Electronics and Communication Engineering, Amrita School of Engineering, Coimbatore, Amrita Vishwa Vidyapeetham, India.
⁴ School of Civil Engineering University College Dublin, Ireland.

PMID: 37683850
DOI: 10.1016/j.scitotenv.2023.166875

Abstract

Suspended sediment concentration (SSC) in water increases temperature and turbidity, limits the photosynthesis of aquatic plants, and reduces biologically available oxygen. It is important to study SSC in the coastal waters of the Arabian Gulf. Thus, this study mapped the SSC of coastal water between Al Arish and Al Ghariyah in northern Qatar using the spectral bands of the MultiSpectral Imager (MSI) of Sentinel-2 by calculating the Normalized Difference Suspended Sediment Index and Normalized Suspended Material Index. The results are studied using the Normalized Difference Turbidity Index and Modified Normalized Difference Water Index. The mapping of SSC in the water using NDSSI showed the presence of a high concentration of suspended sediments between Al Arish and Al Mafjar and a low concentration between Al Mafjar and Al Ghariyah. The mapping of NSMI showed values between 0.012 (clear water) and 0.430 (more suspended material) for the occurrence of suspended materials and supported the results of NDSSI. The study of turbidity using an NDTI image showed turbidity index values ranging from -0.44 (clear water) to 0.12 (high turbidity) and confirmed the occurrence and distribution of suspended sediments and materials in the water. The MNDWI image was able to discriminate clear water with bright pixels from silty sand and mud flats. The relationships between NDSSI, NSMI, and NDTI were correlated with in-situ measurements and studied to find suitable indices to map SSC. Regression analyses showed the strongest relationship between NSMI and NDTI (R² = 0.95) next to NDSSI and NDTI, where NDTI had the strongest effect on NDSSI (R² = 0.86). The satellite data results were evaluated by studying the physical parameters and spatial distribution of suspended sediments in the surface and bottom waters. In addition, the grain size distributions, mineral identification, and chemical element concentrations in the bottom sediment samples were studied.

Keywords: Arabian Gulf; Gulf water; Qatar; Sentinel-2; Spectral indices; Suspended sediment concentration.