For our lab we compared an areal weighting technique and a dasymetric mapping technique. For the areal weighting we estimated the amount of the school aged population per a given high school zone, but that was located outside of areas covered in water. The theory here is that the population could reside anywhere within the census tract as it intersected with the high school zone, as long as that area was outside of a water polygon.
View of impervious areas (in red) as they relate to census tract and high school zones. |
The goal was to determine how many school aged children reside in the impervious areas per high school zone. Each high school area (shown above bounded in dark gray) contains census tract data, but as the view shows the two are not spatially congruent. This also holds true with the impervious areas, which are depicted above in raster format.
To make this all work I ended up using the Zonal Statistics to Table to determine the amount of impervious areas per census tracts. This operation was completed first with my census tract and impervious data, and then again using an intersect of the census tract and high school zone information. New fields were added to each result to account for a 'before' impervious area and an 'after' impervious area. This was important because to ultimately determine the population of school age children per high school zone I used the following calculation: school aged children per high school = total school aged children * ('after' impervious area / 'before' impervious area).
The final result, after error checking against a reference population, showed that only 10% of the population was allocated incorrectly. While not perfect it indicates a slight improvement over the areal weighting technique, which resulted in 11% of the population having been allocated incorrectly.
*Originally published on December 17, 2015. Updated on 2/27/2017 to repair image links.
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