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Grand Mesa, Uncompahgre and Gunnison National Forest Watershed Vulnerability Assessment, Rocky<br />

Mountain Region (R2)<br />

These two scenarios describe a range in climate change predictions that may occur on the GMUG. The<br />

predictions are consistent with the state-wide changes described above, and further refine the potential<br />

effects that may be seen on the GMUG.<br />

Table 1 displays the predicted annual and seasonal changes in precipitation and temperature for the<br />

“moderate” scenario.<br />

Season Precipitation (%) Temperature (˚C) Temperature (˚F)<br />

Annual ~0.0 +2.0 to +3.0 +3.6 to +5.4<br />

Winter +15.0 +2.0 +3.6<br />

Spring -12.0 +2.5 +4.5<br />

Summer -15.0 +3.0 +5.4<br />

Fall +4.0 +2.5 +4.5<br />

Table 1. Temperature and Precipitation Changes for “Moderate” Climate Change Scenario developed<br />

by Barsugli and Mearns for the Gunnison Basin<br />

Predicted changes under the “moderate” scenario include:<br />

1. Increase in annual temperatures of 2-3 ˚C (3.6-5.4 ˚F).<br />

2. No substantial change in annual precipitation, but an increase in cool season precipitation and a<br />

decrease in warm season precipitation.<br />

3. Decrease in annual natural stream flows of 5% to 10%, due to increased temperature, even if<br />

annual precipitation remains the same.<br />

4. Warming temperatures lead to a later accumulation of snow in the fall and earlier snowmelt in the<br />

spring. However, because of the increased precipitation in winter and the generally cold, highelevation<br />

nature of the upper Gunnison basin, the mid-winter snowpack may be similar to the<br />

present.<br />

5. Snowmelt-driven stream flow will occur earlier in the spring by about a week on average. (Note:<br />

this shift is due to warming and does not include the effects of dust-on-snow, which can result in<br />

an even earlier shift in snowmelt.)<br />

6. The earlier melt, along with decreased summertime precipitation and increased summertime<br />

temperatures, results in lower amounts of water stored in the soils during summer and fall.<br />

Table 2 displays the predicted annual and seasonal changes for the “more extreme” scenario. The “more<br />

extreme” scenario is warmer and drier than the “moderate” scenario.<br />

83 Assessing the Vulnerability of Watersheds to Climate Change

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