Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9524896 | Geomorphology | 2005 | 13 Pages |
Abstract
Results show no changes in high flow conditions following impoundment, while low flows are elevated. However, the entire post-dam period is characterized by significantly higher rainfall, which may be obscuring the full impact of flow regulation. Channel activity rates do not indicate a more stabilized planform following dam closure; rather they suggest that the Trinity River is adjusting itself to the stress of Livingston dam in a slow, gradual process that may not be apparent in a modern time scale.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Jessica L. Wellmeyer, Michael C. Slattery, Jonathan D. Phillips,