Here’s Part 1 of Mike Horn’s in-depth look at the problem of dust on snow events and their effects on the snowpack and runoff. His series will include a close look at the Gunnison Basin. From the article:
The new study shows this is due to increased dust caused by human activities in the region during the past 150 years. In addition, peak spring runoff now comes three weeks earlier than before the region was settled and soils were disturbed. Annual runoff is lower by more than 5 percent on average compared to pre-settlement levels…
Tom Painter, a snow hydrologist at both NASA’s Jet Propulsion Laboratory in Pasadena, Calif., and the University of California at Los Angeles, led the research team. His team examined the impact of human-produced dust deposits on mountain snowpacks over the Upper Colorado River basin between 1915 and 2003. Studies of lake sediment cores showed the amount of dust falling in the Rocky Mountains increased by 500 percent to 600 percent since the mid-to-late 1800s, when grazing and agriculture began to disturb fragile but stable desert soils…
The NASA press release explains why dust on snow is such a downer for water supplies. “More than 80 percent of sunlight falling on fresh snow is typically reflected back into space. In the semi-arid regions of the Colorado Plateau and Great Basin, winds blow desert dust east, triggering dust-on-snow events. When dark dust particles fall on snow, they reduce its ability to reflect sunlight. The snow also absorbs more of the sun’s energy. This darker snow cover melts earlier, with some water evaporating into the atmosphere. Earlier melt seasons expose vegetation sooner, and plants lose water to the atmosphere through the exhalation of vapor. The study shows an annual average of approximately 35 billion cubic-feet of water is lost from this exhalation and the overall evaporation that would otherwise feed the Colorado River.
More Gunnison River Basin coverage here.



