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Gallatin National Forest Watershed Vulnerability Assessment, Northern Region (R1)<br />

WATERSHED VULNERABILITY ASSESSMENT PROCESS<br />

Figure 5. The Gallatin National Forest Watershed Vulnerability Assessment Model. The assessment consists of<br />

several different types of information (added and removed as necessary) to identify vulnerable watersheds.<br />

Geophysical/Sensitivity Characterization<br />

The first step of the WVA process, the geophysical/sensitivity characterization, was the most timeconsuming.<br />

As interdisciplinary team (fish biologist, hydrologist, and soil scientist), identified the<br />

dominant physical processes and features of the watershed that affect ecosystem function and condition.<br />

Identifying which watersheds are the most geophysically reactive can indicate how much a watershed<br />

responds to disturbances such as floods, drought, intense precipitation, and fires. The datasets determined<br />

to be most important for the watershed characterization were soils, geology, hydrology, terrain, and<br />

groundwater.<br />

The initial run of this analysis utilized pre-existing datasets (often outdated and of lower resolution and<br />

accuracy). These datasets include the GNF Soil Survey (slope classes, surficial geology, and shallow<br />

groundwater) and datasets derived from the National Hydrography Dataset, National Elevation Dataset,<br />

and R1 VMap (water yield, high flows, and low flows). After this initial run, the team met again to<br />

evaluate the results and determine which watershed characteristics were most important.<br />

The second run of the analysis included newer datasets developed for the analysis. The state surficial<br />

geology layer from MBMG was reclassified into broad rock class categories to identify sensitive<br />

geologies. A compound index of slope and aspect from 10m digital elevation models (USGS) was derived<br />

to identify sensitive terrain areas. The original hydrology metrics were omitted in the second run due to<br />

their strong correlation with the terrain analysis (see Hydrology section below).<br />

Each variable was quantified by subwatershed and given a rating of 1, 2, or 3, based on specific threshold<br />

values identified by literature and professional judgment. All scores were added together by<br />

subwatershed. Higher scores indicate higher sensitivity to disturbance.<br />

Geology Sensitivity<br />

36 Assessing the Vulnerability of Watersheds to Climate Change

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