Floods occur when the stage of water flow exceeds some level, commonly marked by the banks of the stream or river that usually confine the level of flow. What one considers to be a flood is a notion very much limited by human experience, in which observations occur over days, months, or some rather short period of years. In contrast, the timescales of the natural world operate over centuries, millennia, and much longer time periods. When the time scale is enlarged, then the rare occurrence of an extreme flood event can yield magnitudes that seem bizarre relative to the observations made on shorter timescales. The concern of this article will be with those floods that are both rare and of great magnitude. Smaller, common floods are usually considered to be a part of the average process regime of rivers, though lying on the upper tail of the frequency distribution for flow events.
Extreme flood phenomena defy direct measurement in the field. Their recurrence intervals can greatly exceed...
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Baker, V.R. (1978). Floods and other catastrophic events. In: Sedimentology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg . https://doi.org/10.1007/3-540-31079-7_89
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