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Published byLindsay Murphy Modified over 9 years ago
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Shallow Water Bathymetry of Singapore’s Highly Turbid Coastal Waters: A Comparative Approach James F. Bramante, Durairaju Kumaran Raju, Sin Tsai Min Tropical Marine Science Institute, National University of Singapore
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Purpose Determine effectiveness of multispectral algorithms in Singapore Determine how extra 4 bands may help Develop high resolution shallow-water bathymetric map Coral/Benthic Surveys Interface into more complicated IOP models Determine possible new benthic habitats
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Study Area
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Study Area (cont.)
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Marine Environment Study Area (cont.) Wild Singapore Seagrass-watch Pulau Hantu
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Obstacles High turbidity Sediment plumes Few bathymetric data points in shallow waters
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Obstacles (cont.) High shipping traffic Abundant clouds Mixed aerosols from city and ocean
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Atmospheric Correction Stock image (no concurrent field measurements) Access to atmospheric information limited Clear boundaries for cloud, shadowed, and deep ocean pixels
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Atmospheric Correction (cont.) Cloud-shadow empirical algorithm Reinersman et al. (1998) and Lee et al. (2005) Fig. 1 taken from Reinersman et al. (1998)
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Atmospheric Correction (cont.) General Equation: Cloud-Shadow Eq: Assumptions: Lee et al. simplification:
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Atmospheric Correction (cont.) Path radiance: Reflectance: Water-air boundary correction:
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Atmospheric Correction (cont.) Band 2 (Blue) Average Radiance Band 2 Atmospherically Corrected Reflectance
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Bathymetry Algorithms LUT Classification Linear Ratio Algorithm (Stumpf et al. 2003) Linear Band Algorithm (Lyzenga et al. 2006) Compared results using conventional 4 bands and Worldview-2’s 8 bands
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Bathymetry Algorithms (cont.) LUT Classification LUT Library n = 53 for 0 < depth ≤ 2 m Least squares comparison Attempted ratio classification 8-band4-band
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Bathymetry Algorithms (cont.) Linear Ratio Based off of Beer’s law: Stumpf et al. 2003 :
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Bathymetry Algorithms (cont.) Linear Band Lyzenga et al. 2006 : Non-real results when L WCj > L j
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Results Lyzenga et al. AlgorithmBand Classification
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Results (cont.) Lyzenga et al. AlgorithmBand Classification
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Results – Platform Comparison
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Results – Faulty Relationships
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Conclusions With more validation, Lyzenga et al. model and band classifications may prove useful in turbid waters Assumed relationship between band absorption and depth must be re-examined in extremely turbid waters
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Further Investigations Evaluated cloud-shadow atmospheric correction model against RT Model; former was validated and did not affect results much Attempting to use water-column index to adjust for water mass variation in Lyzenga algorithm Using spectroradiometer to modify semi- analytical models for Singapore
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