Publication Information
Title:
| Running dry: Where will the West get its water? |
Author(s): |
Thompson, J. |
Date: |
2007 |
Source: |
Science Findings 97. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 5 p |
Description: |
Late summer streamflow in western and central Oregon and northern California is almost exclusively due to immense groundwater storage in the Cascade Range. The volume of water stored in permeable lava flows in the Cascades is seven times that stored as snow. Nonetheless, until recently, virtually all examinations of streamflow trends under future climates in the West have focused on the anticipated loss of snowpack. This has painted an incomplete picture of the looming water resource crisis that is expected because of global warming. |
Keywords: |
Groundwater, hydrology, Cascade Range, snowpack, climate change, streamflow. |
|
View and Print this Publication (796 KB) |
Publication Notes: |
- We recommend that you also print this page and attach it to the printout of the article, to retain the full citation information.
- This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.
|
|
Get the latest version of the Adobe Acrobat reader or Acrobat Reader for Windows with Search and Accessibility |
|
Citation
Thompson, J. 2007. Running dry: Where will the West get its water?. Science Findings 97. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 5 p
|