Executive
Summary
The primary objective
of this project was to assess the amount of change that occurred between
the years of 1988 to 1993. The region under analysis is a portion of
the Mississippi River watershed. In 1993 a severe flood burdened much
of the area. By comparing the satellite images of the same location
in these two different time periods, an assessment of flood damage can
be interpreted.
Image Processing
Techniques
In order to support the classification of the image, three separate
image-processing techniques were performed. These techniques were the
NDVI, band ratioing, and band combinations. The NDVI index is very effective
in distinguishing land use and land cover in both large and small land
area. Band ratios allow the user to detect and determine specific characteristics
and features of an image. The 3/7 and 4/3 ratios were used.
Classification
Process and Results
Five classes were classified in the miss88.img: Vegetation, Urban Land
Use, Residential, Water, and Barren Land. In the signature editor, the
values for each class in the miss88.img file was set in order from 1-5,
and for the class values for the miss93.img file, the values were to
be multiplied by ten so the values ranged from 10-50.
Accuracy Assessment
Six samples were selected from each class, for example six areas of
vegetation and six areas of residential. In an accuracy assessment of
the miss88 image, the results were more accurate than the flooded image
of miss93. From the five classes the number correct to the total number
is as follows:
1988 image
Total 28/30 = 93%
1993 image
Total 27/30 = 90%
Change Detection
Modeling and Analysis
A model was constructed from the model maker on the ERDAS Imagine model
tab. From the model tools, a raster image tool was selected to represent
the raster layers and included the supervised miss88 image and the supervised
miss93 image as separate layers. The formula created was:
PV x 625
= # of acres changed
4046.86
Through careful calculation,
the total amount of acreage that changed from land to water was determined
to be 12,447.92.