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    Shallow water substrate mapping using hyperspectral remote sensing

    Access Status
    Fulltext not available
    Authors
    Fearns, Peter
    Klonowski, Wojciech
    Babcock, R.
    England, P.
    Phillips, J.
    Date
    2011
    Type
    Journal Article
    
    Metadata
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    Citation
    Fearns, P. and Klonowski, W. and Babcock, R. and England, P. and Phillips, J. 2011. Shallow water substrate mapping using hyperspectral remote sensing. Continental Shelf Research. 31 (12): pp. 1249-1259.
    Source Title
    Continental Shelf Research
    DOI
    10.1016/j.csr.2011.04.005
    ISSN
    02784343
    School
    Department of Physics and Astronomy
    URI
    http://hdl.handle.net/20.500.11937/49219
    Collection
    • Curtin Research Publications
    Abstract

    During April 2004 the airborne hyperspectral sensor, HyMap, collected data over a shallow coastalregion of Western Australia. These data were processed by inversion of a semi-analytical shallow wateroptical model to classify the substrate. Inputs to the optical model include water column constituentspecific inherent optical properties (SIOPs), view and illumination geometry, surface condition (basedon wind speed) and normalised reflectance spectra of substrate types. A sub-scene of the HyMap datacovering approximately 4 km2 was processed such that each 3!3 m2 pixel was classed as sand,seagrass, brown algae or various mixtures of these three components. Coincident video data werecollected and used to estimate substrate types. We present comparisons of the habitat classificationsdetermined by these two methods and show that the percentage validation of the remotely sensedhabitat map may be optimised by selection of appropriate optical model parameters. The optical modelwas able to retrieve classes for approximately 80% of all pixels in the scene, with validation percentagesof approximately 50% for sand and seagrass classification, and 90% for brown algae classification. Thesemi-analytical model inversion approach to classification can be expected to be applied to any shallowwater region where substrate reflectance spectra and SIOPs are known or can be inferred.

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