HR: 08:15h
AN: H11F-02 INVITED [Abstracts]
TI: Space-time integration to assess ecological response to river restoration efforts
AU: * Power, M E
EM: mepower@berkeley.edu
AF: University of California, Berkeley, Department of Integrative Biology, University of California,
Berkeley, Berkeley, CA 94720
United States
AU: Wilcock, P
EM: wilcock@jhu.edu
AF: Johns Hopkins University, Geography & Environmental Engineering
Johns Hopkins University
3400 N. Charles St, Baltimore, MD 21218
United States
AU: Dietrich, W E
EM: bill@eps.berkeley.edu
AF: University of California, Berkeley, Department of Earth and Planetary Science, University of California,
Berkeley, Berkeley, CA 94720
United States
AU: Palen, W
EM: wpalen@berkeley.edu
AF: University of California, Berkeley, Department of Integrative Biology, University of California,
Berkeley, Berkeley, CA 94720
United States
AU: Bode, C
EM: collin@berkeley.edu
AF: University of California, Berkeley, Department of Integrative Biology, University of California,
Berkeley, Berkeley, CA 94720
United States
AB:
To detect impacts of restoration measures on populations or ecosystem processes in rivers and watersheds, we must 1) relate
local changes in state across the watershed to trajectories over time at downstream receiving points; and 2) distinguish
responses to restoration measures from background fluctuations. Both tasks are challenging because of the extreme spatial
heterogeneity and complex dynamics of watersheds and watershed processes over potentially relevant scales that range from
seconds to centuries and mm2 to 1000's of km2. Despite these challenging realities, environmental
scientists and managers are asked to assess the status and responses of riverine ecosystems following restoration efforts
with modest, or no support for watershed-scale monitoring. Here we discuss selected research results that document temporal
and spatial scales of responses to structural changes in channels by processes that underpin food webs that deliver ecosystem
goods or services to society. The trajectories of some types of responses (e.g. uptake and detoxification or outgassing of
pollutants) may be detectable over relatively short time scales (months or years); but others (population trajectories of
resident salmonids) may require decades of monitoring before the magnitude and direction of effects are clear. We also
discuss how new remote and in situ sensing technologies, and ongoing combinations of low and high tech approaches, could
support the expanded monitoring programs that will be essential for realistic evaluations of the long-term efficacy of river
restoration measures.
DE: 0439 Ecosystems, structure and dynamics (4815)
SC: Hydrology [H]
MN: Fall Meeting 2005