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First, peak streamflow should exceed the threshold for a 2-year flood, typically considered as a bankfull condition18. The two-year flood is determined by fitting annual maximum streamflow into a log-Pearson Type III distribution, which is a conventional method used by the U.S. Geological ...
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Higher and/or more frequent flood flows could increase bank erosion, cause greater-magnitude bed-elevation changes (aggradation or scouring, depending on local flux gradients), and alter channel planform through new avulsions (e.g., Macklin & Lewin, 2008; Tucker & Slingerland, 1997). Large ...