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<br />_ <br /> <br />" <br /> <br />e <br /> <br />I <br />1_ <br /> <br />The approaches used include regional frequency analysis, continuous <br />precipitation-runoff analysis with historical precipitBtion data, and <br />single-event precipitation-runoff analysis using synthetic precipitation <br />data. These three general approaches are discussed in this chapter. There <br />are other widely used procedures, such as USGS nomographs, empirical <br />equations, and others. The reader is referred to McCuen, et al. (1977) for a <br />list of references on other methods. <br /> <br />2,1 Generalized Rainfall-Runoff Relations <br /> <br />Hydrograph analysis concepts may be applied to ungaged watersheds <br />through the development and application of generalized functions for <br />estimating the amount of precipitation lost due to interception and <br />infiltration (loss rates), unit hydrographs, and base flow. The unit <br />hydrograph is usually assumed to give a unique relationship between rainfall <br />excess and surface runDff for a basin regardless of storm size, losses, or <br />other factors (Hydrologic Engineering Center, 1973c). Because of its ease of <br />use, the unit hydrograph has received the most attention by hydrologists. <br />However, other methods of hydrograph generation are also becoming widely used <br />(Feldman, 1979), such as the kinematic wave approach to basin modeling, also <br />a feature of HEC-l, Both the unit hydrograph and the kinematic wave analyses <br />will be discussed in this report. <br /> <br />The determination of loss rates is a major problem because loss rates <br />are extremely variable and are dependent on both precipitation patterns and <br />basin characteristics. As a consequence, there is a tendency to adopt a <br />"criteria" approach where loss rates are chosen on the basis of policy rather <br />than being computed. The criteria approach is most appropriate for computing <br />large floods (from synthetic rainfall) r such as floods for spillway design, <br />since losses tend to be small relative to rainfall for large and rare <br />events. This approach is less appropriate when it is used to compute runoff <br />for a range of flood events for system performance evaluations, due in part <br />to the fact that different combinations of rainfall intensities and loss <br />rates can yield similar runoff quantities. <br /> <br />Relating loss rates and analytical loss-rate functions to soil type, <br />land use and cover, antecedent precipitation, and rainfall intensity can be <br /> <br />5 <br />