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<br />8 <br /> <br />ALLUVIAL FAN FLOODING <br /> <br />": <br /> <br />and local public officials (see Box I-I). The committee's approach involved examining the <br />hydrologic and geomorphologic processes that characterize flooding on alluvial fans in a range of <br />varied environments. Understanding these processes from a natural science perspective <br />provides the committee's basis for evaluating how current NFIP practice might be improved to <br />better characterize flood hazards and to more accurately delineate zones of flood risk. The <br />committee's revised definition of alluvial fan flooding is presented in this chapter. Later chapters <br />provide an overview of flood and sedimentation processes on alluvial fans (Chapter 2), describe <br />field indicators and methods to delineate hazard boundaries based on the revised definition <br />(Chapter 3), and give examples of applying the field indicators to specific sites (Chapter 4). <br />Chapter 5 presents the committee's conclusions and recommendations. <br />Because the establishment of this committee was requested by FEMA, that agency and its <br />consultants are the primary audience for this report. However, the committee hopes that <br />communities participating in the NFIP, other agencies, and floodplain management professionals <br />in general will also appreciate this effort to better manage natural hazards in alluvial fan <br />environments. <br /> <br />ORIGIN OF THE PROBLEM <br /> <br />Following a series of damaging floods in the southwestern part of the United States during <br />the 1970s, FEMA sought a new approach to flood risk assessment in areas where flow paths are <br />difficult to predict. Pictures of these floods are shown in FEMA Document 165 (FEMA, 1989), <br />and the images are memorable (see Figure I-I): water and debris flows along new paths not <br />anticipated by planners and residents of the normally dry landscape, automobiles crushed by <br />boulders, a house full of sand. These pictures depict a type of natural hazard different from <br />ordinary riverine flooding. The hazard on active alluvial fans is less foreseeable, more difficult to <br />control or resist, and more dangerous. <br />Many of the pictures in FEMA Document 165 are of flooding on alluvial fans. The term <br />applied by the NFIP to this image was alluvialfal/flooding, and the purpose of Document 165 <br />was to explain how such floods occur. As our understanding changes of how floods occur, <br />regulators develop new policies that eventually become formalized by the writing of regulations. <br />Special rules were thus promulgated to regulate development and to set insurance premiums in <br />areas subject to alluvial fan flooding. Conflict arose when Flood Insurance Rate Maps (FIRMs) <br />prepared by contractors to FEMA were criticized by some participating communities. Most <br />criticism focused on the underlying assumption (or "default assumption") in the FEMA <br />procedure that flooding on alluvial fans is completely unpredictable, an assumption that is not <br />always appropriate (French et aI., 1993). <br /> <br />I <br /> <br />The Problem of Delineating Flood Hazards on Alluvial Fans <br /> <br />Faced with an increased need to map flood risk on alluvial fan areas in the I970s and <br />1980s, and needing a method that can be applied at reasonable expense, FEMA adopted an <br />analytical technique proposed by Dawdy (1979). The procedure uses a general mathematical <br />formula (known as the conditional or total probability equation) to describe the probability of an <br />