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Chapter 10:Hazard Analysis—Floods <br /> 10.3.1 Regional Hazards <br /> Annual rainfall on the island of Hawaii ranges between 300 inches on the slopes of Mauna <br /> Kea above Hilo, to below 10 and 20 inches in the and regions around Kawaihae and South <br /> Point. As expected, flooding is rather common on the wet, windward side of the island where <br /> high annual rainfall is the norm. Most of the flooding that has caused damage has been flash <br /> flooding during extreme rainfall events that bring about sheet flow between stream channels. <br /> In addition, the soils along the Hamakua Coast readily absorb precipitation - thereby <br /> facilitating mudslides and landslides. The Hilo and Puna areas are probably the most <br /> frequently flooded and hardest hit by flash floods on the Big island and perhaps in the <br /> State.51 Perhaps more surprising is the degree of flooding experienced by the more and <br /> regions of the Big Island. The Kohala and Kona districts have a long and active history of <br /> flooding largely due to flash flooding and intense storms. More recently, the South Kohala <br /> and Waikoloa areas have experienced intense flash flooding that has caused considerable <br /> damage.'` <br /> 51 Fletcher,C,B.Richmond,E.Grossman,A.Gibbs,Atlas of Natural Hazards in the Hawaiian Coastal Zone, <br /> Prepared in cooperation with University of Hawaii,State of Hawaii Office of Planning,and National <br /> Oceanic and Atmospheric Administration,U.S.Geological Service Geologic Investigations Series 1-2761, <br /> 2002. <br /> 52 Ibid. <br /> 10-8 Hawaii County Multi-Hazard Mitigation Plan <br />