Abstract
ABSTRACT Observations and measurements were made during storm periods at mountain top sites in the Colorado Rockies during the winter of 1981‐1982. On average, liquid clouds occurred with and without snowfall for, respectively, 75 percent and 15 percent of the observations. On average, the rime ice deposition rates were measured to be seven times the precipitation rates. The rime deposits were estimated to contribute 10 percent to the water content of the snowpack. Combining this figure with the estimated rime deposits on falling snow crystals (up to 50 percent by mass), up to 60 percent of the water content of the annual snowpack in the mountains near Steamboat Springs, Colorado, could be due to rime ice deposits.
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