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<br />SAN MIGUEL, DOLORES. ANIMAS, AND SAN JUAN RIVER BASINS <br />as of February 1, 2000 <br /> <br />Mountain Snow pack" (inches) <br /> <br />I, <br /> <br />~Currenl -'-Average <br />___Maximum --+-Minimum <br /> <br />45 <br /> <br /> <br />) <br /> <br />40 <br /> <br />35 <br /> <br />.5 30 <br />.. <br />c <br />.. <br />OJ 25 <br />> <br />';; <br />g 20 <br /> <br />.. <br />.!! <br />.. 15 <br />== <br /> <br />10 <br /> <br />5 <br /> <br />o <br />Jan Feb Mar Apr May Jun <br /> <br />*Based on selected stations <br /> <br />Precipitation" (% of average) <br /> <br />I_Monlhly DYear-lo-date ] <br /> <br />120 <br /> <br /> <br />100 <br /> <br />.. <br />'" 80 <br />l!! <br />.. <br />> <br />c( <br />'0 60 <br />- <br />c <br />.. <br />u <br />.. <br />.. 40 <br />II. <br /> <br />20 <br /> <br />o <br /> <br />Oct Nov Dee Jan Feb Mar Apr May <br /> <br />These basins managed to pick up nearly average amounts of snowfall during January, which has <br />boosted their combined snowpack accumulation from only 17% of average on January 1, to 41 % <br />of average on February 1. The snowpack percentages are highly variable throughout the basins <br />ranging from only 23% of average in the San Juan Watershed, to 68% of average in the San <br />Miguel Watershed. There is only 47% of the amount of snow in the basin's there was last year at <br />this time. There was 114% of average precipitation during January, but the water year total is <br />now only 34% of average. The combined reservoir storage level in these basins is 116% of <br />average for this time of year, but without an improved snowpack this could easily turn to below <br />average storage during the upcoming runoff season. There is 17 % more storage than last year at <br />this time. All of the forecasted streamflows for this runoff season remain below average and most <br />are lower than last month. Forecasts range from only 31 % of average on the Navajo River at <br />OSO Diversion, to 66% of average at the San Miguel River near Placerville. <br />