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<br />COLUMBIA BASIN -- Continued <br /> <br />to be 36.1 million acre-feet or 110 percent of normal for <br />the January-September period. <br /> <br />Reservoir storage Is excellent. <br />was above normal in all aress and <br />meet summer water supply needs. <br /> <br />Storage 8S of April 1 <br />should be adequate [0 <br /> <br />GREAT BASIN <br /> <br />The \later supply outlook. for the Great Basin Is for <br />much above normal runoff ["angina from 105 percent in the <br />Truckee-Tahoe Basin to over 700 percent for the local <br />inflow on the Lower Sevier River at Gunnison. Most <br />streams are forecsst between 125 to 225 percent of <br />average. The Kumbolt River Bas!n is an area of major <br />concern for the spring runoff season. with predictions <br />near 300 percent of average. Also. high inflows to both <br />Utah Lake and the Great Salt Lake are likely to push <br />these large bodies of water to higher levels than last <br />year, and to levels not previously experienced in almost <br />a century. <br /> <br />March precipitation waa generally near normal state <br />wide but the heaviest area was over the Heaver and Sevier <br />Basin in south central Utah where some reports were in <br />excess of 150 percent of normal. Seasonal precipitation, <br />October through March, is generally 120 to 150 percent <br />over most of the state. Extreme southern areas of Utah <br />are less than HU percent of normal but the northwest <br />corner of Utah and the Sevier River drainage have <br />received amounts in excess of 150 percent. Seasonal. <br />October through March. precipitation amounts this year <br />have exceeded previous observations over the last 50 <br />years at such locations as Ogden Pioneer Power House. <br />Farmington USU, Minersvllle. and Kanosh. <br /> <br />Snowfall during March was nesr normal over northern <br />Utah, above average in central portions of the state, and <br />below normal over extreme southern areas. Some average <br />baain snowpacks include: Hear River--I27 percent, <br />Logan--119 percent, Ogden--153 percent, Weber--135 <br />percent, Jordan--128 percent, Provo--129 percent, <br />Beaver--146 percent, Upper Sevier--95 percent, and Lower <br />Sevier--172 percent. <br /> <br />Some rock and mud slides have slready occurred along <br />the Wasatch front and the threat of additional slides <br />through the snowmelt period is very real. Observed <br />streamflow continues to reflect the saturated aoil <br />conditions and high ground water flow. The seven index <br />station6 measured by the USGS in Utah averaged 146 <br />percent for the month, and since October 1 have averaged <br />167 percent. <br /> <br />The elevation of the Great Salt Lake on April 1 was <br />4207.35 MSL. a rise of 0.65 feet in the las t month. The <br />lake is expected to rise another 1 to 1.5 feet to a level <br />of 4208.0 to 4209.0 feet HSL early this summer. Utah <br />Lake was 3.40 feet above compromise, a rise of 0.20 feet <br />in the last month and is expected to rise an additional <br />1.5 to 2.5 feet by late spring. The flood potential for <br />this spring IS snowmelt has changed very little in the <br />last month and continues to look threatening. April <br />through July forecasts indicate runoff volu~s slightly <br />less than those which occurred last year. <br /> <br />COLORADO BASIN <br /> <br />The water supply outlOOK ranges from below normal in <br />portions of central Arizons to much above normal along <br />the Colorado main stem. The potential for some spring <br />snowmelt flooding. is still high along the east slope of <br />the Wasatch Range in Utah, the Lower Gunniaon Basin, and <br />the San Miguel, and Uncompahgre and Plateau Creek <br />drainages in Colorado. Low lying areas along streams <br />with moderate or higher volumes may also experience SOIDE! <br />runoff problems. <br /> <br />Precipitation during March was quite varied ranging <br />from less than 30 percent over IDOst of Arizona, to nearly <br />twice normal at spotty locations in western Colorado. <br /> <br />Some average baain precipitation amounts for March <br />include: Green River above Flaadng Gorge--90 percent, <br />Upper Colorado River--135 percent. snd the San Juan <br />8asin--85 percent. Seasonal precipitation, October <br />through March, ranges from 75 percent of normal over <br />Arizona 'to greater than 150 percent over portions of <br />weatern Colorsd~~. <br /> <br />March snowfall was near normal over much of the Upper <br />Colorado. Some average basin anowpacka include: Upper <br />Colorado main stem--141 percent. Gunnison drainage--137 <br />percent, San Jusn 8asin--ll1 percent, Yampa and White <br />Rivera--12Z percent, and the Green River above Flaming <br />Gorge Reservoir--83 percent. April 1 snow surveys <br />revealed that new water content records were established <br />for 21 snow courses. Moat of the new records were in the <br />Gunnison and Colorado River watersheds. <br /> <br />Saturated soils, snowmelt, and spring rains may <br />produce aome rock or mud slides on steep slopes. The wet <br />soil and ample ground water conditions are well supported <br />by the continued high flow on the Colorado and Green <br />River drainages since the start of the water year. <br /> <br />Reservoir storage remains high with the combined <br />storage of ten major reservoirs above Lake Powell of 5.9 <br />million acre-feet, 74 percent of capscity. 134 percent of <br />average. and about 250.000 acre-feet lower than last year <br />at this time. Storage in Lake Powell is 21.06 million <br />acre-feet. 84 perc.ent of cspacity and about 1.5 million <br />acre-feet lower than last year at this time. The <br />April-July inflow forecast to Lake Powell is 11.5 million <br />acre-feet. 154 percent of the 20-year, 1961 to 1980 <br />average. <br /> <br />RIO GRANDE BASIN <br /> <br />The predicted water supply outlook varies from IU5 to <br />156 percent of average in the Colorado portion of the <br />basin and from 95 to 185 percent of norms 1 in New Mexico. <br /> <br />Weather conditions during the month of March were very <br />erratic producing variable amounts of precipitation <br />across the basin. The San Luis Valley of Colorado <br />received the greatest amounts which were near 2 to 2.5 <br />times average. The San Juan Mountains area was below <br />normal with amounts as low as 50 percent of average <br />reported. However, some areas of the Sangre De Cristos <br />of northern New Mexico received] times normal. October <br />through March seasonal totals are now near normsl over <br />most of the basin. <br /> <br />Snowfall for the month of Msrch was slightly below <br />normal over all but the eastern areas in the Sangre De <br />Cr!stos of southern Colorado and northern New Mexico and <br />isolated areas of the San Juan Mountains along the <br />Colorado-New Mexico border where amounts of up to 3 times <br />normal were observed. Snowpack is now 115 percent of <br />aversge in the basin in Colorado which is slightly higher <br />than last year at this time. In the New Mexico portion <br />of the basin, 130 percent of average is on the ground <br />which is around 10 percent lower than last year at this <br />time. <br /> <br />Reservoir storage continues well above normal and is <br />about equal to levels observed at this time last year. <br /> <br />ARKANSAS BASIN <br /> <br />The water supply outlook for the ArKanaas <br />is for sbo.ve normal runoff ranging from <br />percent of the 20-year (1961-1980) average. <br /> <br />River Badn <br />135 to 165 <br /> <br />Total precipitation amounts for the mnth of March <br />were much above normal over most of the basin. The atorm <br />track that was established across the area late in the <br />month of February continued through March producing <br />precipitation amounts of 150 to 200 percent of average <br />over the eastern half of the basin, with amounts nesr <br />three times average being reported. Seasonal <br />precipitation totals, October through March, now range <br />from 70 percent in isolated areas of the northern valley <br />to near normal along the southern tributaries. <br /> <br />2 <br /> <br />. . . .continued on page 6 <br />