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Historical and Projected Coastal Louisiana Land Changes

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Figure 15. 1990 to 2000 spatial trend data set in the vicinity of Calcasieu Lake in southwestern <strong>Louisiana</strong>.<br />

Because of the scale of the available images, several years of shoreline erosion <strong>and</strong> internal<br />

marsh degradation may occur before the loss is detectable by using L<strong>and</strong>sat TM based trend<br />

analysis. However, visual examination of multiple dates of TM imagery using remote sensing<br />

software clearly shows the slow degradation of wetl<strong>and</strong>s. Small isl<strong>and</strong>s disappear <strong>and</strong> ponds<br />

increase in size or coalesce to become larger ponds. Any such small gains experienced between<br />

1990 <strong>and</strong> 2000 cannot be considered in this analysis but are unlikely to alter the trends <strong>and</strong><br />

patterns identified here.<br />

Error Assessment<br />

Classification Accuracy<br />

Classification accuracy assessments were performed on the 1999 <strong>and</strong> 2002 L<strong>and</strong>sat TM imagery<br />

to quantify the reliability of the data sets. The accuracy assessments were performed by an<br />

experienced image interpreter who was not involved in the classification of the source TM<br />

imagery. A stratified r<strong>and</strong>om sampling approach was used to create an equal number of<br />

sampling points for the l<strong>and</strong> <strong>and</strong> water classes merging each data set to provide overall accuracy.<br />

20

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