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Discovery
Dust-on-Snow: On Spring Winds, Something Wicked This Way Comes

Earlier snowmelt, altered water supplies, result

Photo showing zebra stripes of dust and snow on the snow surface in Colorado mountains.

"Zebra stripes" of dust and snow are visible on the snow surface in Colorado mountains.
Credit and Larger Version

April 2, 2010

On spring winds, something wicked this way comes.

At least for the Colorado Rocky Mountains and their ecosystems, as well as people who depend on snowmelt from these mountains as a regional source of water.

"More than 80 percent of sunlight falling on fresh snow is reflected back to space," says Tom Painter, Director of the University of Utah's Snow Optics Laboratory. "But sprinkle some dark particles on the snow and that number drops dramatically."

That's exactly what's happening in Colorado's high peaks.

When the winds are right and the desert is dry, dust blows eastward from the semi-arid regions of the U.S. Southwest. In a dust-up, Western style, small dark particles of the dust fall on Colorado's pristine white snowfields.

"The darker dust absorbs sunlight, reducing the amount of reflected light and in turn warming the now 'dirty' snow surface," says scientist Chris Landry, Director of the Center for Snow and Avalanche Studies (CSAS) in Silverton, Colo.

Painter's and Landry's research on dust-on-snow events, as they're called, is supported by the National Science Foundation's (NSF) division of Atmospheric and Geospace Sciences, which is part of the directorate for geosciences.

Dust-on-snow events, long recognized as a phenomenon, were little understood despite frequent and regionally extensive dust deposition, says Painter.

Although scientists knew from theory and modeling studies that this dust changed the albedo--the solar energy absorption properties--of snowfields, no one had made measurements of its full impact on snowmelt rates.

Then during the winter/spring of 2004, Painter and Landry began their project.

They were the first to make systematic measurements of dust-on-snow events along with complementary climate and hydrologic data.

"Painter's and Landry's observations have confirmed--and most importantly quantified--what many snow and climate scientists had hypothesized but only tested in models," says Jay Fein, program director in NSF's Division of Atmospheric and Geospace Sciences.

Spring snowmelt from the Rocky Mountains provides much of the American West's water supplies. As a result of Painter's and Landry's research, water managers have gained new insights into the snowmelt process, and are applying those findings through the Colorado Dust-on-Snow (CODOS) program.

CODOS is based at the Center for Snow and Avalanche Studies.

Landry's discussions with water managers led to the development of CODOS, now funded by local, regional, state and federal water management agencies.

CODOS monitors the statewide distribution of dust in mountain snow cover and reports on that distribution in biweekly advisories.

It provides timely analyses of how the dust affects snowmelt timing and rates, and is continuing research driven, in part, by stakeholder questions.

Twelve dust-on-snow events during the winter of 2008/2009 led to a 40 to 50 day earlier snowmelt--which occurred 20 days earlier than normal--with record streamflow rates.

CODOS's monitoring and forecasting services made all the difference, says Fein, enabling water managers to anticipate these events and still provide reliable water supplies.

Wicked, dust-laden winds, already moving westward this spring, no longer blow unfettered. The work of Tom Painter and Chris Landry stands in their way.

--  Cheryl Dybas, NSF (703) 292-7734 cdybas@nsf.gov

Related Websites
Center for Snow and Avalanche Studies: http://www.snowstudies.org/

Photo of CSAS Director Chris Landry measuring snow water equivalence in a snowpit.
CSAS Director Chris Landry in June, 2007, measuring "snow water equivalence" in a snowpit.
Credit and Larger Version

Photo of scientist Tom Painter tracking radiation in June, 2007.
Scientist Tom Painter tracking radiation in June, 2007; in melting snow, dust comes to light.
Credit and Larger Version

Photo of CSAS researcher Andrew Temple in Colorado's San Juan Mountains on May 12, 2009.
CSAS researcher Andrew Temple in Colorado's San Juan Mountains on May 12, 2009.
Credit and Larger Version

Photo showing dust layers in a study plot in Colorado's Senator Beck Basin Study Area.
Twelve dust layers in a study plot in Colorado's Senator Beck Basin Study Area.
Credit and Larger Version

Photo of University of Utah researchers Annie Bruyant and McKenzie Skiles in Wolf Creek Pass, Colo.
University of Utah researchers Annie Bruyant and McKenzie Skiles in Wolf Creek Pass, Colo.
Credit and Larger Version



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