For this week’s exercise we focused on two methods of presenting data on an isarithmic map: continuous and hypsometric. We used PRISM annual precipitation data obtained from the USDA NRCS National Geospatial Management Center in coordination with the PRISM Group at Oregon State University for the state of Washington from 1981-2010.
First, we created a map presenting the precipitation data in
continuous form. We also created our own hillshade layer to add to our map
display elevation since this effect hasn’t been added to ArcGIS pro yet. Then
we created a second map in which we converted the data to a hypsometric tint to
better visualize the precipitation totals. To do this we used the Int (Spatial
Analysis) tool to convert the raster data to integers. We then created 10
manual intervals to classify the data. We added our hillshade layer and added
contour lines using the Spatial Analysis Contour List to add contour values. Finally,
we were tasked to create a map layout and to include a description of how the
data was interpolated.
When reviewing the differences in the continuous and hypsometric
maps and answering the process summary questions I was
reminded of a recent map I’d viewed on my local weather station’s website. Sure
enough, both the tornado risk and predicted precipitation totals were shown on
a hypsometric isarithmic map similar to the one I created.

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