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Chugach National Forest Watershed Vulnerability Assessment, Alaska Region (R10)<br />

Eyak Lake Resurrection Creek<br />

Air Temperature °C<br />

Annual Mean Annual Mean<br />

A1B Scenario B1 Scenario A1B Scenario B1 Scenario<br />

2000-2009 4.3 3.5 1.4 0.5<br />

2020-2029 5.1 4.4 2.1 2.1<br />

2050-2059 6.1 5.3 3.1 2.4<br />

Cordova January Hope January<br />

2001-2010 -1.4 -3.3 -6.1 -8.2<br />

2031-2040 -0.2 0.7 -5.2 -4.2<br />

2061-2070 2.3 0.2 -2.3 -4.7<br />

Cordova July Hope July<br />

2001-2010 14.1 13.1 15.1 14.1<br />

2031-2040 14.3 14.4 15.2 15.4<br />

2061-2070 15.6 14.9 16.7 15.9<br />

Table 2. Predicted changes for annual mean air temperatures for the Eyak Lake and Resurrection Creek watersheds<br />

as a whole, and selected monthly temperatures for the towns of Cordova and Hope.<br />

Annual mean precipitation is generally predicted to increase, although the total amounts are quite<br />

different for the two watersheds. As shown in Table 3, the increase in the Eyak Lake watershed as a<br />

whole is predicted to be as much as 6.7 inches under the A1B scenario, while the Resurrection Creek<br />

watershed may see an increase of 3.1 inches. The data for the driest and wettest months for Cordova and<br />

Hope were taken from the SNAP community charts (2011), and generally show small increases over time.<br />

Unlike the other trends, the prediction for June 2061-2070 shows a slight decrease, but given the<br />

variability among the models used for the prediction (University of Alaska, Fairbanks 2011), this is<br />

probably not significant.<br />

It should also be mentioned that the historic annual precipitation levels are highly variable for the<br />

Cordova area. The Cordova airport weather station, which is about 10 km from the Eyak Lake watershed,<br />

has an annual mean of 96.26 inches, but a historic range of 54.41 to 139.34 inches. Thus, while an<br />

average annual increase of six inches will lead to higher flows and presumably more extreme events, the<br />

watershed already experiences extreme changes. This makes it difficult to determine how, or how much,<br />

geophysical and biological conditions will be affected.<br />

From 1979 to 1995, a low-elevation station near Hope had a precipitation range of 15.19 to 31.30 inches,<br />

with a mean of 22.15 (Kalli and Blanchet 2001). The predicted amounts for the entire watershed are<br />

higher as shown below, but the predicted changes still appear well within the historic range.<br />

Eyak Lake Resurrection Creek<br />

Precipitation Inches<br />

Annual Mean Annual Mean<br />

A1B Scenario B1 Scenario A1B Scenario B1 Scenario<br />

2000-2009 177.2 176.9 34.5 38.0<br />

2020-2029 179.6 178.3 35.8 38.1<br />

2050-2059 183.9 179.0 37.6 39.8<br />

Cordova June Hope May<br />

2001-2010 7.81 7.52 0.85 0.89<br />

2031-2040 7.86 7.50 1.05 0.96<br />

2061-2070 7.70 7.69 1.14 1.01<br />

Cordova October Hope September<br />

2001-2010 21.13 20.83 3.52 3.73<br />

2031-2040 21.92 21.19 3.68 3.50<br />

2061-2070 22.10 21.23 4.47 3.97<br />

275 Assessing the Vulnerability of Watersheds to Climate Change

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