18.01.2013 Views

watervulnerability

watervulnerability

watervulnerability

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Shasta Trinity National Forest Watershed Vulnerability Assessment, Pacific Southwest Region (R5)<br />

Figure 7. Trends in snow depths from snow courses on the Shasta-Trinity National Forest. Maximum, mean and<br />

minimum depths are shown in green, blue and red, respectively.<br />

Figure 8. Photographs of the Hotlum Glacier, Mount Shasta, taken September 18, 1935 (left) and August 24, 2008<br />

(right). Photos courtesy of Mount Shasta Climbing Rangers.<br />

APPROACH TO ASSESSING VULNERABILITY<br />

The general model used in this assessment is shown in Figure 9. The approach starts with identifying<br />

important aquatic resource values on the Forest that might be affected by climate change. Next, the<br />

potential changes to climate and the resources were assessed. The third step was to examine factors that<br />

might modify the response. The three components are characterized (rated and ranked) at the watershed<br />

scales described above. Vulnerability was derived by overlaying the products of the first three steps.<br />

The objective of the assessment was to provide a means of describing relative vulnerability of aquatic<br />

resources on the Forest to potential climate change impacts. It is important to remember the results are not<br />

applicable to watersheds not on the Forest, and they are not based on ecological thresholds.<br />

192 Assessing the Vulnerability of Watersheds to Climate Change

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!