Ap. Georgakakos et al., IMPACTS OF CLIMATE VARIABILITY ON THE OPERATIONAL FORECAST AND MANAGEMENT OF THE UPPER DES-MOINES RIVER BASIN, Water resources research, 34(4), 1998, pp. 799-821
Data from the regulated 14,000 km(2) upper Des Moines River basin and
a coupled forecast-control model are used to study the sensitivity of
flow forecasts and reservoir management to climatic variability over s
cales ranging from daily to interdecadal. Robust coupled forecast-cont
rol methodologies are employed to minimize reservoir system sensitivit
y to climate variability and change. Large-scale hydrologic-hydraulic
prediction models, models for forecast uncertainty, and models for res
ervoir control are the building blocks of the methodology. The case st
udy concerns the 833.8 x 10(6) m(3) Saylorville reservoir on the upper
Des Moines River. The reservoir is operated by the U.S. Corps of Engi
neers for flood control, low-flow augmentation, and water supply. The
total record of 64 years of daily data is divided into three periods,
each with distinct characteristics of atmospheric forcing. For each cl
imatic period the coupled forecast-control methodology is simulated wi
th a maximum forecast lead time of 4 months and daily resolution. For
comparison, the results of operation using current reservoir control p
ractices were obtained for the historical periods of study. Large diff
erences are found to exist between the probabilistic long-term predict
ions of the forecast component when using warm or cool and wet or dry
initial conditions in the spring and late summer. Using ensemble input
corresponding to warm or cool and wet or dry years increases these di
fferences. Current reservoir management practices cannot accommodate h
istorical climate variability. Substantial gain in resilience to clima
te variability is shown to result when the reservoir is operated by a
control scheme which uses reliable forecasts and accounts for their un
certainty. This study shows that such coupled forecast-control decisio
n systems can mitigate adverse effects of climatic forcing on regional
water resources.