Table 10. Significant changes to environmental flow components in the McKenzie River basin as a result of upstream dams.
[Reaches 8 and 10 were not evaluated for changes because of the Leaburg and Walterville canal diversions, respectively]
Reach No. |
Large floods |
Small floods |
High flows |
Low flows |
Extremely low flows |
Monthly distribution |
1 |
Less frequent |
Less frequent |
No significant change |
No significant change |
No significant change |
No significant change |
2 |
No significant change |
No significant change |
No significant change |
No significant change |
No significant change |
No significant change |
3 |
Eliminated |
Decreased magnitude,
less frequent |
Decreased magnitude |
Increased magnitude |
Increased magnitude, shift in timing from September to March |
Decreased streamflow from February to May, increased streamflow from July to November |
4 |
Decreased magnitude |
Decreased magnitude |
No significant change |
Increased magnitude |
Increased magnitude,
no significant change in timing. |
Decreased streamflow from February to May, increased streamflow from August to November |
5 |
Eliminated |
Eliminated |
No significant change |
Increased magnitude |
Increased magnitude, shift in timing from September to March |
Decreased streamflow from February to May, increased streamflow from July to November |
6, 7 |
Decreased magnitude, less frequent |
Decreased magnitude, less frequent |
No significant change |
Increased magnitude |
Increased magnitude, no significant change in timing. |
Decreased streamflow from March to May, increased streamflow from July to November |
9, 11, 12 |
Decreased magnitude, less frequent |
Decreased magnitude, less frequent |
No significant change |
Increased magnitude |
Increased magnitude, no significant change in timing. |
Decreased streamflow from March to May, increased streamflow from July to November |
|
First posted February 8, 2010
Part or all of this report is presented in Portable Document Format (PDF); the latest version of Adobe Reader or similar software is required to view it. Download the latest version of Adobe Reader, free of charge. |