Temporal analysis of remotely sensed turbidity in a coastal archipelago |
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Affiliation: | 1. Department of Biological and Environmental Engineering, Cornell University, Ithaca, NY, USA;2. School of Civil and Water Resources Engineering, Bahir Dar University, Bahir Dar, Ethiopia;3. Geospatial Data and Technology Centre, Bahir Dar University, Bahir Dar, Ethiopia;4. Department of Civil and Environmental Engineering, Cornell University, Ithaca, NY, USA;5. Department of Earth and Environment, Florida International University, Miami, FL, USA;1. Agro-Meteorology Division, National Institute for Agro-Environmental Sciences, 3-1-3 Kannondai, Tsukuba, Ibaraki 304-8604, Japan;2. Technische Universität Dresden, Institute of Hydrology and Meteorology, Chair of Meteorology, Dresden D-01062, Germany;3. The National Laboratory for Agriculture and the Environment (USDA-ARS-NLAE), 2110 University Blvd, Ames, IA 50011, USA;4. European Commission, Joint Research Centre, Institute for Environment and Sustainability, Ispra, Italy;5. Institute of Geography, University of Cologne, Cologne 50923, Germany;6. Agrosphere Institute (IBG-3), Institute of Bio- and Geosciences, Jülich 52425, Germany;7. Fundación Centro de Estudios Ambientales del Mediterráneo (CEAM), Charles Robert Darwin, 14, Parque Tecnológico, Paterna 46980, Spain;8. INRA, UMR INRA-AgroParisTech ECOSYS, Thiverval-Grignon 78850, France;9. CESBIO (CNES/CNRS/UPS/IRD), 18, Avenue Edouard Belin, Toulouse Cedex 9 31401, France |
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Abstract: | A topographically fragmental archipelago with dynamic waters set the preconditions for assessing coherent remotely sensed information. We generated a turbidity dataset for an archipelago coast in the Baltic Sea from MERIS data (FSG L1b), using CoastColour L1P, L2R and L2W processors. We excluded land and mixed pixels by masking the imagery with accurate (1:10 000) shoreline data. Using temporal linear averaging (TLA), we produced satellite-imagery datasets applicable to temporal composites for the summer seasons of three years. The turbidity assessments and temporally averaged data were compared to in situ observations obtained with coastal monitoring programs. The ability of TLA to estimate missing pixel values was further assessed by cross-validation with the leave-one-out method. The correspondence between L2W turbidity and in situ observations was good (r = 0.89), and even after applying TLA the correspondence remained acceptable (r = 0.78). The datasets revealed spatially divergent temporal water characteristics, which may be relevant to the management, design of monitoring and habitat models. Monitoring observations may be spatially biased if the temporal succession of water properties is not taken into account in coastal areas with anisotropic dispersion of waters and asynchronous annual cycles. Accordingly, areas of varying turbidity may offer a different habitat for aquatic biota than areas of static turbidity, even though they may appear similar if water properties are measured for short annual periods. |
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Keywords: | Remote sensing Ocean colour Turbidity Time series Temporal averaging The Baltic Sea Archipelago Coast |
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