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White River National Forest Watershed Vulnerability Assessment, Rocky Mountain Region (R2)<br />

Figure 9. Climate change vulnerability rating for the Infrastructure/Roads resource value. Red shading depicts<br />

subwatersheds with the highest vulnerability. Road-stream crossings are shown as blue dots.<br />

As expected, the lower elevation subwatersheds are those that display the highest vulnerability to a<br />

changing climate. These are the watersheds with lower precipitation, more area in the rain-snow transition<br />

zone, and an absence of glaciated terrain. Because of the low elevation, these subwatersheds also tend to<br />

have a large private-land component and the highest number of irrigation diversions.<br />

Note that even as the resource value changes, there is not a huge variability in the mapped outcome. The<br />

natural and anthropogenic factors do not radically change, which supports the notion of minimizing the<br />

number of resource values considered. In this case, two resource values areas could have sufficed: One<br />

that captures effects from decreasing low flows (droughts) and one that captures increasing high flows<br />

(floods).<br />

APPLICATION<br />

Focus on Anthropogenic Influences<br />

As a whole, management activities on National Forests don’t create a lot of greenhouse gasses. So instead<br />

of focusing on the causes of climate change, our concern might center on increasing the resiliency of our<br />

landscapes to minimize their negative response to climate change. Looking back at the analysis process<br />

used, our role in increasing resiliency is ultimately very narrow, because much of a subwatershed’s<br />

126 Assessing the Vulnerability of Watersheds to Climate Change

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