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<br />often been accompanied by simultaneous, more destructive floods <br />on the Arkansas River. The descriptive accounts of Arkansas River <br />flooding appear to dominate such historic records as are available <br />for the region. <br /> <br />* <br /> <br />* <br /> <br />* <br /> <br />INTERMEDIATE REGIONAL FLOODS on Fountain Creek are floods that have <br /> <br /> <br />an average frequency of occurrence in the order of once in loo years. <br /> <br /> <br />They are determined from analyses of floods that have occurred on <br /> <br /> <br />Fountain Creek and other streams in the general area. <br /> <br />* <br /> <br />* <br /> <br />* <br /> <br />STANDARD PROJECT FLOODS are floods which would be exceeded only on <br /> <br /> <br />rare occasions and are reasonably characteristic of the geographical <br /> <br /> <br />area in which the drainage basin is located. In many instances, <br /> <br />they may define the upper limit of flooding against which protec- <br /> <br /> <br />tion may be sought. The Standard Project Fluod Dn'Fountain Creek <br /> <br />would average about 7 feet higher than the Intermediate Regional <br /> <br /> <br />Flood along most of the stream. <br /> <br />* <br /> <br />* <br /> <br />* <br /> <br />FLOOD DAMAGES resulting from either the Intermediate Regional Flood <br /> <br /> <br />or the Standard Project Flood would be more extensive than from <br /> <br /> <br />past floods because of increased development in the flood plain, <br /> <br /> <br />and the wider extent, greater depths, and higher velocities of <br /> <br /> <br />flood waters. <br /> <br />* <br /> <br />* <br /> <br />* <br /> <br />MAIN FLOOD SEASON. Analysis of climatological data and inspection <br /> <br /> <br />of the flood history for the Arkansas River subbasin above John <br /> <br /> <br />Martin Dam show that the most severe flood-producing storms occur <br /> <br /> <br />during the late spring or summer months. The spring season is the <br /> <br /> <br />transitional period between the occurrence of instability and fron- <br /> <br /> <br />tal activity and is subject to storms caused by both types of ac- <br /> <br /> <br />tivities or a combination thereof. Also, the movement and interac- <br /> <br /> <br />tion between airmasses during these seasons are more pronounced. <br /> <br /> <br />This may result in heavy spring snow storms in the higher elevations <br /> <br /> <br />or in high intensity rains during the spring. These storms and the <br /> <br />2 <br />