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<br />- <br /> <br />I <br /> <br />I <br /> <br />-I <br /> <br />I <br /> <br />1 <br /> <br />features are typical of a mountain valley on an eastern slope near the <br /> <br /> <br />central port~on of a large continent. They include low prec1p1~ation, <br /> <br /> <br />low humidity, abundant sunshine, a wide daily temperature range, and <br /> <br /> <br />generally low winds. The surrounding mountains act as a barrier prevent- <br /> <br />ing the northern cold air or eastern storms from penetrating the Upper <br /> <br />Arkansas River Valley. <br /> <br />I <br /> <br />CHAPTER III <br /> <br />1 <br /> <br />HISTORY OF FLOODING <br /> <br />1 <br /> <br />1 <br /> <br />1 <br /> <br />Streamflow records are available at locations near and within the <br />study reaches. Recorded historical flows show maximum discharges of <br />1,110 and 307 cfs for the South Arkansas River at Poncha and Poncha Creek <br />at Poncha Streamflow Recording Stations. These flows were recorded on <br />July 5, 1911 and May 27, 1912, respectively. Long term streamflow records <br />from nearby stations indicate that peak flows occurred in a number of <br />years, particularly in 1957. <br /> <br />1 <br /> <br />The records at the Salida weather station, elevation 7060 feet, show <br /> <br />an average annual precipitation of 10.87 inches. precipitaiton varies <br /> <br /> <br />at Salida from less than 8 inches in one year out of six to over 15 inches <br /> <br /> <br />in one year out of six. The highest recorded annual precipitation was <br /> <br />17.92 inches in 1961. This was followed by the lowest annual precipitation <br /> <br /> <br />on record, 4.91 inches in 1962. The monthly distribution of precipitation <br /> <br /> <br />varies considerably from one year to the next. Dry months (less than one- <br /> <br /> <br />quarter inch of precipitation) are rare for April, July and Augus,t. Wet <br /> <br /> <br />months (more than 2 inches precipitation) occur about one in four years in <br /> <br /> <br />July, one in five years in April and August. Summer thunderstorms account <br /> <br /> <br />for almost 59 percent of the annual precipitation, and account for local <br /> <br /> <br />high flows. Hail falls occasionally in the study area. <br /> <br />I <br /> <br />1 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The documentation of the peak flows in the study area included: <br />research of the past issues of Salida newspapers, personal interviews <br />with the local residents who have resided in the area for a long period, <br />discussions with the city and county officials, and a written solicitation <br />from the Colorado Water Conservation Board requesting input from a number <br />of local residents who were identified by the local officials as possible <br />sources of information on the history of flooding of the South Arkansas <br />River and Poncha Creek. <br /> <br />1 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Summers are cool in the study area with temperatures reaching into the <br /> <br /> <br />90's a few times each summer. A maximum temperature of 1000 F was recorded <br /> <br /> <br />in August 1902. Temperatures for the summer nights usually drop below <br /> <br /> <br />500 F. Winter temperatures, particularly in the daytime, are usually <br /> <br /> <br />warmer than those found at similar or lower elevations. Periods of extreme <br /> <br /> <br />c~ld temperatures are of short duration. The lowest temperature recorded <br /> <br /> <br />at Salida was 3D' F below zero 1n January 1919. The average annual tempera- <br /> <br /> <br />ture is 46.50 F , and the average summer temperature is 62.6'F. The average <br /> <br /> <br />frost free period is approximately 107 days. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />II <br />i <br />I <br /> <br />The research of the past 1ssues of the <br />Mailll were centered around specific dates. <br /> <br />Salida newspaper "Mountain <br /> <br /> <br />These dates were selected from <br /> <br /> <br />eleven streamflow gaging stations <br /> <br />dates include: <br /> <br />a review of a graph of peak flow data for <br />near the study area. Specifically, these <br /> <br />I <br /> <br />I <br /> <br />May 21, 1901 <br /> <br />July 8, 1952 <br /> <br />I <br /> <br />Because of the climatic conditions, the irrigated land in the vicinity <br /> <br /> <br />of the study area is in meadows, native hay, and alfalfa. The area is better <br /> <br /> <br />adapted to livestock production as compared with farming. Dryland farming <br /> <br />is almost nonexistent in the upper reaches of the Arkansas River Basin. <br /> <br />I <br /> <br />June 5, 1911 <br /> <br />June 29, 1957 <br /> <br />I <br /> <br />June 12, 1921 <br /> <br />July I, 1957 <br /> <br />I <br /> <br />July 17, 1923 <br /> <br />June 6, 1958 <br /> <br />-9- <br /> <br /> <br />June 16, 1924 <br /> <br />June 20, 1965 <br /> <br />I <br /> <br />June 21, 1947 <br /> <br />July 13, 1965 <br /> <br />I <br /> <br />June 10, 1952 <br /> <br />June 11, 1973 <br /> <br />I <br /> <br />-10- <br />