This week, the cartography lab focused on creating an isarithmic
map of average annual precipitation in Washington State using a variety of
raster symbology techniques. The data came from the PRISM Climate Group and was
downloaded from the USDA Geospatial Gateway. There are many methods for interpolating climate data from monitoring
stations to grid points. While some perform well in flat terrain, few
effectively capture the complex climatic variations found in mountainous areas.
PRISM addresses this challenge by incorporating a conceptual framework that
accounts for orographic effects such as elevation, aspect, and slope. Precipitation
data collected between 1981 and 2010 in Washington was interpolated using
the PRISM Model (Parameter-elevation Regressions on
Independent Slopes Model), which blends monitoring station data with a digital
elevation model (DEM) to generate a
climatological average over the 30-year period, to account for topographic
variations that occur in mountainous regions.
Continuous Tones
Continuous
tone symbology is a method of displaying raster data where values are
represented with a smooth gradient of colors, rather than distinct classes or
categories. This symbology method is useful for showing continuous data, like
precipitation, where values change gradually across space. The initial raster,
“precipann_r_wa,” was brought into ArcGIS Pro and symbolized using a continuous
tone color ramp specific to precipitation. To enhance the surface
visualization, I added a ‘hillshade effect’, which uses elevation to
visually emphasize terrain, in ArcGIS Pro via the hillshade function.
The result was a smooth and natural-looking precipitation surface.
Hypsometric Tints
To move from continuous to discrete symbology, I used
the Int tool to convert the raster’s values into integers. This allowed
me to classify the data into 10 equal intervals using the Classify option
in the Symbology pane. Each range is a distinct color from the precipitation
ramp to create hypsometric tints, a method that divides elevation or continuous
data (in this case, precipitation) into visually distinct color bands. The
combination of the precipitation symbology and the legend makes the spatial
distribution of rainfall easier to interpret at a glance.
Overlay Contours
As hypsometric tins cannot be displayed
without contour lines, I then added overlaying contour lines using the Contour List Spatial Analyst tool. Using the “Annual Precipitation (in)”
raster dataset for the input layer, I manually added contour elevations in the Contour Value Fields that matched the 10 classes displayed in the
hypsometric tint symbology classes creating a “Contours” output dataset. Contours
help reinforce the boundaries between precipitation zones and add another
visual cue for interpreting variation in the data. With both contours and tints
overlaid, the map clearly shows the relationship between precipitation patterns
and elevation, especially in areas with steep terrain.
Summary
This lab was a fun exercise in translating
complex, continuous climate data into a readable and visually engaging map. By
walking through different symbolization techniques (continuous tone, hypsometric
tinting, and contours), I gained a better understanding of how to
tailor symbology to different data types and mapping goals.




