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Location: Great Lakes Environmental Research Laboratory
2205 Commonwealth Blvd.
Ann Arbor, MI 48105-2945
Date: Friday, October 30th, 1998
Time: 10:00 am
Room: 105 (Main Conference Room)
Dr. Efi Foufoula-Georgiou,
of the Department of Civil Engineering, University of Minnesota, will be presenting a talk
entitled "Space-time rainfall organization and its role in validating
quantitative precipitation forecasts" on Friday, October 30th at
10:00 am in the main conference room of the NOAA Great Lakes Environmental Research Laboratory,
Ann Arbor, Michigan.
Dr. Foufoula-Georgiou's major research interests are in the area of stochastic
modeling of surface and subsurface hydrologic processes and systems. Specific
areas of research include stochastic modeling of space-time rainfall using
rain gauge, radar, and satellite data; estimation of exceedance probabilities
of extreme design events; geomorphologic study of river networks and hydrologic
response; optimal operation of water resources systems under uncertainty;
and monitoring network design.
Her current research focuses on studying and understanding the statistical
structure of hydrologic processes at a range of scales of interest to
hydrology, and developing a theoretical framework for multi-scale analysis
of stochastic processes. Of particular interest are remotely sensed rainfall
fields and river network structures.
Several studies have presented evidence for the presence
of scale-invariance in spatial, temporal or spatio-temporal rainfall patterns.
Such an organization in observed patterns is hoped to be also statistically
reproduced in patterns predicted by atmospheric numerical weather prediction
models. However, this idea has not yet been explored for assessment of
the predictive skill of atmospheric models and for validation of quantitative
precipitation forecasts (QPFs). This talk reviews evidence of space-time
organization in observed rainfall and advocates the need to develop new
multiscale measures of forecast performance, i.e., measures that can depict
how well the scale-to-scale variability (be that scale-invariant or not)
of the forecasted fields matches that of the observed fields. We demonstrate
that these measures are more informative and provide valuable feedback
for atmospheric model improvements as compared to traditional measures
of QPF verification.
Last updated: September 19, 2002 mbl
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