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<br /> <br />METHOD FOR ESTIMATING THE MAGNITUDE AND <br /> <br />FREQUENCY OF FLOODS AT UNGAGED SITES ON <br /> <br />UNREGULATED RURAL STREAMS IN IOWA <br /> <br />By Oscar G. Lara <br /> <br />ABSTRACT <br /> <br />This report provides techniques and procedures for estimating the <br />probable magnitude and frequency of floods at ungaged sites on Iowa <br />streams. Physiographic characteristics were used to define the boundaries <br />of five hydrologic regions. Regional regression equations that relate the <br />size of the drainage area to flood magnitude are defined for estimating <br />peak discharges having specified recurrence intervals of 2, 5, 10, 25, 50, <br />and 100 years. Regional regression equations are applicable to sites on <br />streams that have drainage areas ranging from 0.04 to 5,150 square miles <br />provided that the streams are not affected significantly by regulation <br />upstream from the sites and that the drainage areas upstream from the sites <br />are not mostly urban areas. Flood-frequency characteristics for the <br />mainstems of selected rivers are presented in graphs as a function of <br />drainage area. <br /> <br />INTRODUCTION <br /> <br />This report represents the fourth update in the last 33 years of the <br />magnitude and frequency of floods in Iowa. Flood reports were updated to <br />provide more dependable flood-data and more accurate and reliable methods <br />for estimating the magnitude and frequency of floods. These estimates are <br />needed to implement efficient flood-plain management strategies and for <br />economical design of highway structures, levees, and buildings in the flood <br />plain. Economic design criteria require the availability of adequate data <br />with long periods of record, improved analytical methods, and better <br />understanding of the flood hydrology of Iowa. <br /> <br />The first of three previous reports (Schwob, 1953) was limited to an <br />analysis of the magnitude and frequency of floods that was based on data <br />collected in Iowa before 1950. A second report (Schwob, 1963) included <br />updated data and a method for estimating magnitude and frequency of floods <br />at sites on ungaged rural streams that had drainage areas of 10 square <br />miles or more. The third report (Lara, 1973) was prepared using data <br />updated through 1972. This report also included a method for estimating <br />the magnitude and frequency of floods at sites on ungaged rural streams <br />that had drainage areas of two square miles or more. <br /> <br />1 <br />