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  • ACRS 1999


    Hyper Spectral Image Processing
    Simulated Spot-Equivalent Reflectance Characteristics of Common Reef Features

    Analysis of Variance
    A statistical procedure for analyzing data with a quantitative dependent variable and a categorical independent variable, as is the case here, is analysis of variance (ANOVA). The variance of means is compared to the background variance of the data from which the means are determined. In the following one-way ANOVA, the null hypothesis of equal sample means is tested against the alternative hypothesis that each bottom type category comprises a separate population. ANOVA procedures compare differences in means such that within- and between-group variability are compared and referenced to the grand mean of the dataset.

    An analysis of variance was performed on the entire dataset consisting of 596 SPOT 1 reflectance values (dependent variable) separated into 5 groups (healthy coral, bleached coral, algae, rubble and sea grass) with the null hypothesis that the means of all 5 groups are equal. In performing the ANOVA, the goal is to determine what part of the variance should be attributed to randomness and what part can be attributed to other factors. The Mean Square (MS) column reveals the sum of squares divided by the degrees of freedom, which indicates variance. The first value, 0.09, measures the variance between groups, while the second value, 0.00, measures the variance within groups. Since the variance between groups is larger than the variance within groups, then the average bottom reflectance is not the same for each group.

    The F-value, 21.03, is the ratio of the two variances and is used to choose between the two hypotheses where the null hypothesis will be rejected if the F-ratio is in the upper 5% of the F distribution. The p-value is 0.00, which is less than the alpha value of 0.05 specified as the confidence level. The null hypothesis that the group means are equal must therefore be rejected at the 5% level. The calculated F-statistic, 21.03, is greater than the F-critical value, 2.39, indicating that the calculated F-statistic is in the upper 5% of the F-distribution. Therefore, although the qualitative assessment and comparison of population means suggested that there were no discernible differences, the statistical results of ANOVA suggest that the reflectance measurements were taken from 5 different or unique populations.

    4. Conclusions
    There is little qualitative difference between in situ reflectance values of various substrates collected at depth in a coral reef environment. This indicates that visual interpretation of remotely sensed imagery will yield inaccurate classification results. Significant mixing of several different substrate types within the relatively large pixels of SPOT HRV images (20x20m) compounds the issues of classification inaccuracy. Other complicating factors include the effects of attenuation and multiple scattering from the overlying water column, refraction of light at the air-water interface, scattering and absorption in the atmosphere, and effects of the variable morphology of the substrate with respect to slopes and self-shading.

    The results of the statistical analysis of the simulated SPOT HRV reflectance values are encouraging since the populations can be considered significantly and sufficiently different to allow discrimination. While the populations defined for this study are admittedly broad, the categorization will still be useful for a change detection study of a large geographic region. Due to the natural variation of reflectance values both within and between populations, accurate and definite identification of substrate type may not be advisable especially considering the additional sources of error when the values are sensed remotely rather than in situ, as in this study. Alternatively, the fact that the in situ data reveals statistical separability between populations suggests that change detection is the most appropriate use of currently available satellite imagery.

    Although the satellite imagery available has significant limitations in the accuracy and precision with which it can be used to map and monitor changes in coral reef ecosystems, the overt changes that are occurring warrant the use of the technology in an attempt to further our understanding of coral reefs. The currently available passive satellite imagery with appropriate spectral band locations (visible wavelengths for water penetration) should therefore be utilized to map the geographic extent of coral reefs and investigate changes in ecosystem health. The errors associated with the coarse spatial, spectral and temporal resolution should not be ignored, but rather, attempts should be made to minimize the associated errors and communicate the limitations of the digital image analysis results.

    References
    • Bour, W., Loubersac, L. and Rual, P. 1986. Thematic mapping of reefs by processing of simulated SPOT satellite data: application to the Trochus niloticus biotope on Tetembia Reef (New Caledonia). Marine Ecology Progress Series. 34, 242-249.
    • de Vel, O. and Bour, W. 1990. The Structural and Thematic Mapping of Coral Reefs Using High Resolution SPOT data: application to the Tetembia Reef, New Caledonia. Geocarto International, 2, 27-34.
    • Hardy, J., Hoge F., Yungel, J. and Dodge, R. 1992. Remote Detection of coral Bleaching Using Pulsed-Laser Fluorescence Spectroscopy. Marine Ecology, 88, 247-255.
    • Holden, H. 1999. An analysis of in situ observations of spectral reflectance characteristics of coral reef features in Fiji and Indonesia. Technical Report, Waterloo Laboratory for Earth Observations, University of Waterloo, Waterloo, Ontario, Canada, 206pp.
    • Holden, H. and LeDrew, E. 1998a. Spectral discrimination of healthy and non-healthy corals based on cluster analysis, principal components analysis and derivative spectroscopy. Remote Sensing of Environment. 65, 217-224.
    • Holden, H. and LeDrew E. 1998b. The scientific issues surrounding remote detection of submerged coral ecosystems. Progress in Physical Geography. 22 (2), 190-221.
    • Holden, H. and LeDrew, E. In Press. Hyperspectral identification of coral reef features. International Journal of Remote Sensing.
    • Jupp, D, K. Mayo, Kuchler, D., Claasen, D., Kenchington, R. and Guerin, P. 1985. Remote Sensing for Planning and Managing the Great Barrier Reef of Australia. Photogrammetria, 40, 21-42.
    • Luczkovich, J., Wagner, T., Michalek J., and Stoffle R. 1993. Discrimination of coral reefs, seagrass and sand bottom types from space: a Dominican Republic case study. Photogrammetric Engineering and Remote Sensing. 59 (3), 385-389.
    • Muller-Parker, G. and D’Elia, C. 1997. Interactions between corals and their symbiotic algae. In Life and Death of Coral Reefs. C. Birkeland (ed.). International Thompson Publishing: New York. 536 pages.
    • Mumby, P., Green, E., Clark, C. and Edwards, A. 1998. Digital analysis of multispectral airborne imagery of coral reefs. Coral Reefs 17, 59-69.
    • Myers, M., J. Hardy, C. Mazel, and P. Dustan. 1999. Optical spectra and pigmentation of Caribbean reef corals and macroalgae. Coral Reefs. 18, 179-186.
    • Wilkinson, C., Linden, O., Cesar, H., Hodgson, G., Rubens J., and Strong, A. 1999. Ecological and socioeconomic impacts of 1998 coral mortality in the Indian Ocean: an ENSO impact and a warning of future change? Ambio. 28 (2), 188-196.
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