Ecohydrologic Analysis of a Riverine
and Reservoir-Fringe System: A Case Study in Support of Reservoir Management
Efforts
by Mark Rains, University of California at Davis
ABSTRACT
In the United States, there are more than 75,000 dams greater than
six feet in height, and the reservoirs created by these dams cover approximately
three percent of the land surface. Most reservoirs are managed exclusively
for traditional purposes: municipal and irrigation water supply, hydroelectric
power, flood control, and recreation. However, there is growing interest
in managing reservoirs, at least in part, for the maintenance of plant
and wildlife habitats. Most of the discussion surrounding this management
objective is centered on the downstream effects of reservoir operations.
Thus, decommissioning dams or otherwise restoring natural flow regimes
has been the focus of many recent efforts. This approach, however, does
not always clearly result in net ecosystem benefits since reservoir-fringes
often support regionally-unique plant communities that serve as critical
habitats for regionally-uncommon wildlife species. Decommissioning dams
or otherwise altering reservoir operations may restore some channel and
floodplain functions but may degrade or eliminate these regionally-unique,
reservoir-fringe ecosystems.
In this project, we explore how reservoir operations affect riverine
and reservoir-fringe ecosystems upstream of East Park Reservoir on the
east front of the Coast Range, California. The overall objective of this
project is to develop concepts and tools for the planning, implementation,
and monitoring stages of regional reservoir management efforts. First,
we use isotopic and chemical procedures to identify the seasonally-varying
sources of shallow ground water. Shallow ground water is recharged primarily
by stream water and regional ground water, with regional ground water by
far the more prominent source in the dry season. Second, we use hydrometric
procedures to identify the key boundary conditions governing shallow ground
water. A ground-water backwater effect caused by the reservoir extends
up valley under the delta and reduces the impacts of regional ground water
pumping on the shallow ground water resources. Third, we use a linked ground-water
and vegetation distribution model to simulate conditions under alternative
reservoir operations. Simulated vegetation distributions on the delta differ
markedly under alternative reservoir operations, though some of the regionally-unique
plant communities persist even under the full drawdown scenario.
Seminar held February 3, 2003 at New Mexico Tech, at 3:15 pm, MSEC
103
Sponsored by Hydrology Program