Stream Recurrence intervals: An important question for hydrologists, urban planners, land-use experts, and home owners to consider is "how frequently does a river overflow its banks and cause a flood?" The bar graph below of discharge values shows that the Gunnison River (1975-1995) reached a 3600 cfs discharge rate in 1990. It's important to know how often this rate will occur. Or, how often can we expect a much more serious flood event of perhaps, 6000 cfs?

The answer to these questions involves simple statistics that begin with the idea of the Recurrence Interval (RI) of a flood. RI is the average number of years between peak discharge values of a certain size. For example a river may overflow its banks on an average of once in 30 years with a discharge of at least 6000 cfs. Thus, the Recurrence Interval (for a 6000 cfs flood) is 30 years. It should be pretty obvious to you that in order to determine RI for different sized floods, we need to examine a stream's discharge over many years.

The first step in determining Recurrence Interval is to make up a table of a stream's annual peak discharge data. Using the data of the graph above, complete the table below of Annual Peak Discharge values for the Gunnison River. Some values are determined for you.

Year
Q (cfs)
Year
Q (cfs)
Year
Q (cfs)
Year
Q (cfs)
Year
Q (cfs)
1975
200
1979
100
1983
2100
1987
1.
1991
5.
1976
300
1980
900
1984
1700
1988
2.
1992
6.
1977
1250
1981
250
1985
1200
1989
3.
1993
7.
1978
500
1982
950
1986
1350
1990
4.
1994
8.
               
1995
9.

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