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<br />General Rain Floods <br />General rain floods can result from moderate to heavy rainfall occurring over a wide <br />geographic area lasting several days. They are characterized by a slow steady rise in <br />stream stage and a peak flood of long duration. As various minor streams empty into <br />larger and larger channels, the peak discharge on the mainstream channel may progress <br />upstream or downstream (or remain stationary) over a considerable length of river. <br />General rain floods can result in considerably large volumes of water. The general rain <br />flood season is historically from the beginning of May through October. Because the rate <br />of rise is slow and the time available for warning is great, few lives are usually lost, but <br />millions of dollars in valuable public and private property are at risk. <br /> <br />Thunderstorm Floods <br />Damaging thunderstorm floods are caused by intense rain over basins of relatively small <br />area. They are characterized by a sudden rise in stream level, short duration, and a <br />relatively small volume of mnoff. Because there is little or no warning time, the term <br />"flash flood" is often used to describe thunderstorm floods. The average number of <br />thunderstorm days per year in Colorado varies from less than 40 near the western <br />boundary to over 70 in the mountains along the Front Range. The thunderstorm flood <br />season in Colorado is from the middle of July through October. <br /> <br />Snowmelt Floods <br />Snowmelt floods result from the melting of the winter snowpack in the high mountain <br />areas. Snowmelt floods typically begin as spring mnoff appears, after the first spring <br />warming trend. If the trend continues up to 8 to 10 consecutive days in a basin where the <br />snowpack has a water content more than about 150% of average, serious flooding can <br />develop. The total duration of snowmelt floods is usually over a period of weeks rather <br />than days. They yield a larger total volume in comparison to other types of floods in <br />Colorado. Peak flows, however, are generally not as high as flows for the other types. A <br />single cold day or cold front can intermpt a melting cycle causing the rising water to <br />decline and stabilize until the cycle can begin again. Once snowmelt floods have peaked, <br />the daily decreases are moderate, but fairly constant. Snowmelt flooding usually occurs <br />in May, June, and early July. <br /> <br />Rain on Snowmelt Floods <br />Rain on snow flooding occurs most often in Colorado during the month of May. It is at <br />this time of year that large general rainstorms occur over western Colorado. These <br />rainstorms are most often caused when warm moist air from the Gulf of Mexico begins <br />pushing far enough north that it begins to affect western weather. In combination with <br /> <br />13 <br />