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USGS Water Science Centers are located in each state.

There is a USGS Water Science Center office in each State. Washington Oregon California Idaho Nevada Montana Wyoming Utah Colorado Arizona New Mexico North Dakota South Dakota Nebraska Kansas Oklahoma Texas Minnesota Iowa Missouri Arkansas Louisiana Wisconsin Illinois Mississippi Michigan Indiana Ohio Kentucky Tennessee Alabama Pennsylvania West Virginia Georgia Florida Caribbean Alaska Hawaii New York Vermont New Hampshire Maine Massachusetts South Carolina North Carolina Rhode Island Virginia Connecticut New Jersey Maryland-Delaware-D.C.

Hydrology of Kansas Floods

Located in the central plains, Kansas is affected by the same weather patterns that affect adjoining States. These patterns are dominated by major weather systems that move from west to east across the State. The flow of moisture is seasonal. During winter, moisture originates over the Pacific Ocean and precipitates over the Rocky Mountains; the remaining moisture moves into the State from the northwest and west. Kansas tends to receive less precipitation during winter than summer. During summer, southerly winds move moisture originating over the Gulf of Mexico into the State. Occasionally, remnants of tropical cyclones, including hurricanes originating in the Gulf, move into the State and produce considerable quantities of precipitation.

The nature of these moisture-delivery systems results in numerous, severe floods and long, severe droughts. Since the flood of 1844, the most severe and widespread flood was in July 1951. The 1951 flood, which affected almost one-half of the State, resulted from an intense storm in early July that was preceded by greater than normal rainfall during May and June. Peak discharges in the Kansas, Marais des Cygnes, and Neosho Rivers generally had recurrence intervals greater than 100 years, were greater than any previous discharges, and have not been equaled since. Other significant floods occurred on the Republican River in 1935, the Arkansas River in 1965, the Solomon River in 1973, and the Verdigris River Basin in 1976. Although the storm near Great Bend in 1981 did not affect a large area, its intensity caused severe flooding and considerable damage.

During the spring and summer of 1993 widespread reoccurring rainstorms over the upper Mississippi and Missouri River Basins caused flash flooding and extensive regional flooding. In Kansas, the northeastern half of the State had the worst flooding; however, flood-control reservoirs in Kansas reduced the level of flooding significantly (Perry, 1994). Floods in Kansas during 1993 are documented in "Summary of Floods in the United States, January 1992 through September 1993" (Perry and Combs, 1998).

(Modified from Clement, R.W., 1991, Kansas floods and droughts, in Paulson, R.W., Chase, E.B., Roberts, R.S., and Moody, D.W., compilers, National water summary 1988-89 -- Hydrologic events and floods and droughts: U.S. Geological Survey Water-Supply Paper 2375, p. 287-294.)

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