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

needs to be weighted in order to combine them into a meaningful aggregate score. The processes for<br />

assigning categories and relative weights are as follows.<br />

Determination of High, Moderate, and Low Categories for Subwatershed Attributes<br />

In order to apply a simple mathematical ranking system by subwatershed, each of the previously<br />

discussed attributes required binning into categories. The amount of influence that an attribute exerts<br />

within a given subwatershed was categorized as high, moderate, or low.<br />

Upon inspection, most of the attributes or influences have no physical threshold to suggest a breakpoint<br />

between categories. For example, we don’t have any data to suggest how many diversions per square mile<br />

a subwatershed can contain and still have a low influence on aquatic systems. Since the objective of this<br />

analysis was to determine relative vulnerability between subwatersheds, a simple and objective approach<br />

was used. For each attribute listed, the distribution of the 166 subwatersheds was plotted and the quartiles<br />

determined. By definition, the first quartile is the 25 th percentile of the ranked data, the second quartile is<br />

the median, and the third quartile is the 75 th percentile of the ranked data. Subwatersheds below the first<br />

quartile (lowest 25%) were ranked as low influence; subwatersheds between the first and third quartile<br />

(middle 50%) were ranked as moderate; subwatersheds above the third quartile (top 25%) were ranked as<br />

high. See the example plot for road density below in Figure 6.<br />

Figure 6. A sample histogram of diversions per square mile across all subwatersheds, and the use of quartiles to<br />

categorize the relative influence on resiliency as high, moderate, or low<br />

Determination of the Relative Weights of Inherent and Anthropogenic Attributes<br />

While each of the attributes listed has some effect on the ultimate resiliency of the subwatersheds, they do<br />

not have equal effects. For example, the amount of precipitation or the amount of water withdrawn from a<br />

subwatershed is likely more important than a primary productivity increase from calcareous geology.<br />

Consequently, a simple method of scaling the relative influence of the attributes was developed.<br />

Since physically removing water from the stream (water uses) has the most direct effect on aquatic<br />

systems, each attribute was weighted relative to that, with values ranging from 0.25 (1/4 the effect) to 1<br />

(similar effect). The assigned weights are as follows: geochemistry of parent geology (0.25), extent of<br />

122 Assessing the Vulnerability of Watersheds to Climate Change

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