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Effects of climate change on the hydrology of upper Alameda Creek
Kirk Klausmeyer, University of California, Berkeley
Term project for Landscape Architecture 222, Prof. G. Mathias Kondolf, University of California, Berkeley, Spring 2005.
ABSTRACT: Scientists predict that future climate change will effect both human and natural systems. Using
two rainfall-runoff modeling methods, this analysis predicts the effects of climate change on the
hydrology of upper Alameda Creek, a small drainage area in California’s Coast Range. I
analyzed daily rainfall, temperature, and stream flow data collected from field gages for 8 years
to develop a numerical predictive model. Using the Army Corps of Engineers Hec-HMS model
and autoregressive statistical techniques, I minimized the difference between the predicted and
the observed creek discharge. I then generated an altered temperature and precipitation regime
based on a high-end climate change prediction downscaled to a 60 square mile grid. For upper
Alameda Creek, annual precipitation is predicted to fall by 28.2% and annual temperature is
predicted to increase by 5.2°C by 2100. The autoregressive model had the lowest error when
compared to the observed data, and predicts a 22% decrease in total discharge and considerably
smaller peak flows with climate change. The Hec-HMS model predicts a 46% reduction in total
discharge and large reductions in peak flows with climate change. Reduced discharge and peak
flows will have adverse impacts on downstream uses, including drinking water supplies for San
Francisco, recreational uses at Sunol Regional Wilderness, and habitat for native rainbow trout,
alluvial sycamore, California red-legged frog, California tiger salamander, and other rare and
endangered species.
SUGGESTED CITATION: Kirk Klausmeyer,
"Effects of climate change on the hydrology of upper Alameda Creek"
(May 12, 2005).
Water Resources Center Archives.
Hydrology.
Paper klausmeyer.
http://repositories.cdlib.org/wrca/hydrology/klausmeyer
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