School | Reference Population | Estimated Population | Error | Abs(Error) |
Hagerty | 4706 | 4214 | 492 | 492 |
Lake Brantley | 6313 | 6094 | 219 | 219 |
Seminole | 11776 | 10881 | 895 | 895 |
Winter Springs | 5693 | 3863 | 1830 | 1830 |
Lyman | 7853 | 8477 | -624 | 624 |
Oviedo | 4780 | 4750 | 30 | 30 |
Lake Howell | 8585 | 6561 | 2024 | 2024 |
Lake Mary | 5014 | 4885 | 129 | 129 |
Total: | 54720 | 49725 | 4995 | 6243 |
Accuracy (%): | 11.40899123 |
Monday, April 18, 2016
GIS 5935 Lab 15: Dasymetric Mapping
Dasymetric mapping is essentially breaking down larger aggregations of data into smaller areas or units. It is often used in population density estimates. For example, it could be the process of taking aggregated statewide population data and breaking it down to the county level. This week's assignment was along those lines. For this analysis, I was to take raster data and use its imperviousness to estimate prospective student populations for eight high schools. This was done by joining the raster's zonal statistics table to census vector data, then running an Ordinary Least Squares analysis on that to determine the estimated population. From there, I had to clip the OLS result to each school boundary and determine its area and new estimated population. The results of my estimated population vs. a reference, "true" population can be seen below:
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