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Figure 3.21 Annual Precipitation Norms, 1971 – 2000.<br />

Riverine Flooding<br />

Riverine flooding is defined as <strong>the</strong> overflow of rivers, streams, drains, and lakes due to<br />

excessive rainfall, rapid snowmelt or ice melt. The areas adjacent to rivers and stream banks<br />

that carry excess floodwater during rapid runoff are called floodplains. A floodplain is defined as<br />

<strong>the</strong> lowland and relatively flat area adjoining a river or stream. The terms “special flood hazard<br />

area” and “100-year flood” refer to <strong>the</strong> area in <strong>the</strong> floodplain that is subject to a one percent or<br />

greater chance of flooding in any given year. Floodplains are a larger entity called a basin,<br />

which is defined as all <strong>the</strong> land drained by a river and its branches.<br />

Location<br />

All of Region L is susceptible to flash flooding and riverine flooding. The surface waters of <strong>the</strong><br />

planning area flow through 2 water basins: The Kansas Lower Republican and <strong>the</strong> Marais des<br />

Cygnes as shown in Figure 3.22 shows <strong>the</strong> Marais des Cygnes and Figure 3.23 shows <strong>the</strong><br />

Kansas Lower Republican.<br />

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