Water-Supply Paper 2502Summary of Significant Floods in the United States, Puerto Rico, and the Virgin Islands, 1970 Through 1989Summary of Significant Floods, 1970 Through 1989, by State or TerritoryIn addition to the specific flood data, this section provides a description of the hydroclimatology and a summary of significant floods for each State or territory in the United States. The summary of significant floods includes those with loss of life or excessive damage during the period 1970 through 1989. The floods that were in the top 5 percent of each streamflow-gaging station's record during this period are tabulated, and an estimated recurrence interval is provided along with other pertinent data. A map of each State or territory is supplied to locate the streamflow-gaging stations. IllinoisHydroclimatologyIllinois is located in the midcontinent interior and is affected by various weather patterns during the year. Moisture sources include the Gulf of Mexico, the Pacific Ocean, and, to a small degree, Lake Michigan. Frontal systems are quite active in Illinois as warm humid airmasses from the Gulf of Mexico are displaced by continental polar air from Canada or maritime polar air from the North Pacific Ocean. Winter storms usually become stronger as they cross the State and intensify as a result of temperature differences across the polar front. Mean annual precipitation ranges from 35 in. in the north to 46 in. in the south. Areas within 10 to 20 mi of Lake Michigan are affected by lake-effect snowfall in the winter and have greater annual values of precipitation. During the winter, floods can be caused by ice jams that force localized flooding. Thunderstorms associated with frontal systems and squall lines are responsible for flash flooding in the State during the summer months. Rainfall rates of 16 in. in 12 hours have been recorded from these systems. Persistent upper atmospheric patterns can result in repeating storm systems that can lead to regional flooding. On the basis of regionalization procedures that relate flood characteristics to watershed and climatic characteristics, the magnitude of maximum discharges for streams in Illinois is dependent on drainage area, main-channel slope, and 2-year, 24-hour rainfall (Jennings and others, 1994). Significant FloodsTwenty percent of the streamflow-gaging stations in the State recorded significant discharges during the flood of December 1982. Rainfall in the Illinois River Basin totaling 3 to 5 in. on wet soil caused the flooding. This flood was responsible for eight deaths. During February to March 1985, excessive rain on snow in northern Illinois caused $10 million in damages. From September 20 to October 3, 1986, excessive rains in northern Illinois resulted in four deaths and $50 million in damages. Parts of Chicago were inundated by as much as 9.4 in. of rain on August 13 and 14, 1987, that resulted in four deaths and $77.6 million in damages (Paulson and others, 1991). The location of streamflow-gaging stations in Illinois that had significant floods for 1970-89 is shown in figure 35 and 35a by station number. The specific data for each significant flood are listed in table 14. A significant flood is one that ranks in the top 5 percent of all annual maximum discharges for that station's period of record. References
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