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<br />199B. Colorado F10utI Hazard Mitigation Plan (409) <br /> <br />Floods in June 1983, along the Cache Ia Poudre River <br />in Fort Collins and Greeley; along Clear Creek and ~s <br />tributaries in Silver Plume and Georgetown; and along <br />the Arkansas River in Fremont and Chaffee counties <br />were principally due to melting snow. The 1984 flood~ <br />on the western slope were primarily snowme~ flood- <br />ing. <br /> <br />2.2.1.4 Rain on Snow Floods <br /> <br />Rain on snowme~ flooding occurs most often in Col- <br />orado during the month of May. It is at this lime of year <br />that large general rainstorms occur over westem Col- <br />orado. These rainstorms are most often caused when <br />warm moist air from the Gulf of Mexico begins pushing <br />far enough north that it begins to affect western <br />weather. In combination with this movement of air <br />mass is the continued possibility of cold fronts moving <br />into Colorado from the Pacific Northwest. When these <br />weather phenomena collide, long Iasting'general rain- <br />storms can often occur. Rain on snowmelt exacer- <br />bates an already tenuous situation as snowmelt wa- <br />ters rush down heavily incised stream channels. Any <br />abnormal increase in flow from other sources usually <br />causes streams to leave their banks. <br /> <br />During the spring months of May and June when rivers <br />are running high, there is a potential for flooding due to <br />rain falling on metting snow. Usually such rain is over <br /> <br />a small part of a basin, and the resuiting flood is of <br />short duration and may often go unnoticed in the lower <br />reaches of a large drainage basin. To some extent, <br />the cloud cover associated with the rain system can <br />slow the me~ing cycle and offset the compound effect. <br />In some cases, however, rainfall may be heavy and <br />widespread enough to noticeably affect peak flows <br />throughout the basin. <br /> <br />Flooding along the Colorado River in Grand Junction <br />in July of 1884, along Clear Creek at Georgetown in <br />June of 1965 and along the Gunnison and Colorado <br />rivers at Grand Junction in June of 1983, are examples <br />of fiooding from rain on me~ing snow. The effect of <br />rain on me~ing snow in the Colorado River basin in <br />1983 was fe~ as far downstream as Mexico. In 1984, <br />rain or melting snow caus6d severe flooding condi- <br />tions at Paonia. <br /> <br />On May 28, 1993, rain on snowme~ flooding occurred <br />at Paonia on the North Fork of the Gunnison River. <br />The rainfall occurred over a 5-hour period during the <br />evening. This caused the North Fork of the Gunnison <br />River to reach its highest level since the 1984 flood <br />season. Many miles of agriculture land experienced <br />severe bank erosion in unincorporated Delta County. <br />The stone riprap at Paonia's wastewater treatment <br />plant experienced severe damage as did the bank <br />armoring at Huff Addition 31 (a subdivision). A photo <br /> <br /> <br />FIIe:FHMP-Chapter-2.pub <br /> <br />;.-;;,-,-'-,,--.....,..;....,~~~..... <br /> <br />."-' -..' <br />...,-"..-------' <br /> <br />Chapter 2 - 7 <br /> <br />1/27118 6:14 AI8 <br />