Editorial Type:
Article
Article Type:
Research Article

WRF Model Simulation of Two Alberta Flooding Events and the Impact of Topography

Thomas K. Flesch Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada

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Gerhard W. Reuter Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada

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Print Publication:
01 Apr 2012
DOI:
https://doi.org/10.1175/JHM-D-11-035.1
Page(s):
695–708
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Abstract

This study examines simulations of two flooding events in Alberta, Canada, during June 2005, made using the Weather Research and Forecasting Model (WRF). The model was used in a manner readily accessible to nonmeteorologists (e.g., accepting default choices and parameters) and with a relatively large spatial resolution for rapid model runs. The simulations were skillful: strong storms were developed having the correct timing and location, generating precipitation rates close to observations, and with precipitation amounts near that observed. The model was then used to examine the sensitivity of the two storms to the topography of the Rocky Mountains. Comparing model results using the actual topographic grid with those of a reduced-mountain grid, it is concluded that a reduction in mountain elevation decreases maximum precipitation by roughly 50% over the mountains and foothills. There was little sensitivity to topography in the precipitation outside the mountains.

Corresponding author address: Thomas Flesch, Dept. Earth and Atmos. Sci., University of Alberta, Edmonton AB T6G2E3, Canada. E-mail: thomas.flesch@ualberta.ca

Abstract

This study examines simulations of two flooding events in Alberta, Canada, during June 2005, made using the Weather Research and Forecasting Model (WRF). The model was used in a manner readily accessible to nonmeteorologists (e.g., accepting default choices and parameters) and with a relatively large spatial resolution for rapid model runs. The simulations were skillful: strong storms were developed having the correct timing and location, generating precipitation rates close to observations, and with precipitation amounts near that observed. The model was then used to examine the sensitivity of the two storms to the topography of the Rocky Mountains. Comparing model results using the actual topographic grid with those of a reduced-mountain grid, it is concluded that a reduction in mountain elevation decreases maximum precipitation by roughly 50% over the mountains and foothills. There was little sensitivity to topography in the precipitation outside the mountains.

Corresponding author address: Thomas Flesch, Dept. Earth and Atmos. Sci., University of Alberta, Edmonton AB T6G2E3, Canada. E-mail: thomas.flesch@ualberta.ca
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