This weeks module covered isarithmic maps. In this lab, we were tasked with creating a precipitation map of Washington state depicted with hypsometric tints, hillshade effect, and contours. Data was acquired from the USDA Geospatial Data Gateway and the PRISM Group at Oregon State University.
In order to show continuous data throughout the map, the data needed to be interpolated. The precipitation data was interpolated using the Parameter-elevation Relationships on Independent Slopes Model (PRISM), which is an analytic tool that uses point-based climate measurements to predict monthly or annual climate behavior. Another useful feature of PRISM is that is accounts for variables in the map such as terrain and elevation by utilizing a digital elevation model (DEM) which enhances the accuracy of climate data.
To complete this map, hypsometric tinting, also known as elevation coloring, was implemented. Hypsometric tinting is used to show elevation differences on a map by using different colors on different elevation ranges. For this map, the hypsometric tinting was implemented by using the geoprocessing tool called Int (Spatial Analyst Tool) and inputting the annual precipitation raster data. Next, contours were overlayed on the hypsometric tints. This was performed using another geoprocessing tool called Contour Listand run using the same annual precipitation raster data.
The result is a map that illustrates how precipitation is impacted by elevation and terrain, which is important for understanding patterns in the climate of any given area.