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<br />Baca County <br /> <br />on the Cirnarron River approximately 10 miles downstream of the Colorado- <br />Kansas state line; it has a drainage area of 2,899 square miles. The elevation <br />of Carrizo Creek ranges from 4,800 to 6,600 feet, while the Cimarron River's <br />elevation at the state line is approximately 3,600 feet. <br /> <br />i <br />I <br />I <br />f <br /> <br />i <br />, <br /> <br />i <br />I <br /> <br />The headwaters of Two Butte Creek lie adjacent to those of Carrizo Creek <br />upstream in Las Animas County. Further downstream in Las Animas <br />County, the Bear Creek headwaters separate Carrizo and Two Butte creeks; <br />Bear Creek eventually flows into the Arkansas River. <br /> <br />4.1.3 Local Flooding Problems <br /> <br />Tributaries in Baca County, induding Carrizo Creek and Cimarron River, <br />historically have experienced nuisance flooding during the summer months <br />because of highly localized storms. However, Two Butte Creek flooded for <br />the first time in 22 years during the storm events of 1997. <br /> <br />The incorporated areas seldom experience significant flooding problems. For <br />example, the Town of Springfield is built near the divide between two creek <br />channels within the Bear Creek watershed and rarely experiences any <br />flooding. <br /> <br />4.1.4 Storm Characteristics <br /> <br />r <br /> <br />Although Baca County experienced widespread flooding during the summer <br />of 1997, the type of storms in the southeastern region of Colorado were at a <br />lower intensity than those observed in the northeastern counties. While <br />counties in northeastern Colorado experienced bullseyes of extreme, <br />short-duration precipitation, the summer storm pattern in Baca County <br />produced numerous storms with moderately heavy rainfall over a few days. <br />Table 4.1-1 summarizes those storms that produced over 1 inch of rain in a <br />24-hour period in July and August of 1997. <br /> <br />r <br />~ <br />I <br /> <br />Although the storms in the latter two dates caused damaging floods, limited <br />information is available for these storms. Therefore, the primary focus of this <br />discussion is on the storm that produced rainfall through the evening hours <br />of August 5 and into the morning of August 6. While the entire county <br />witnessed some rainfall, the precipitation intensity was greatest south of <br />Walsh and down through Stonington. <br /> <br />The nearest weather station that recorded multiple types of atmospheric data <br />is located 51 miles northwest of Walsh in the Prowers County Seat, Lamar. <br />Daily data was collected at this station for each of the four events identified <br />in Table 4.1-1. A summary of this data is presented in Table 4.1-2. <br /> <br />d479/chaP4-1.doc 08/12/98 <br /> <br />4.1-3 <br />