Quasi-equilibrium conditions of urban gravel-bed stream channels in southern Ontario, Canada, and their implications for urban-stream restoration
Urban gravel-bed stream channels in southern Ontario, Canada, identified to be in a state of quasi-equilibrium have been studied over the past 15 years and compared against rural gravel-bed stream channels of the same hydrophysiographic region. Bankfull width and depth versus bankfull discharge were not found to increase as a function of increasing urbanization as has been found in many other studies. The observed annual frequency of bankfull discharge was typically less than a 1-year return period with many sites ranging between two to eighteen bankfull events per year with higher intensity ...
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