11-12

During last weekend's beautiful weather, small delicate facets formed throughout SW Montana near the snow surface.  After Friday's snowfall they were buried and preserved in most places creating a new weak layer in the snowpack.  The grid in the background is 1-2 mm in size.  These particular crystals are called radiation recrystallized facets photographed by the YC Ski Patrol conducting avalanche research with the Engineering School at MSU.

Northern Madison, 2012-02-11

GNFAC Avalanche Advisory for Thu Feb 9, 2012

Snowpack and Avalanche Discussion

The southern Madison and southern Gallatin Ranges, the Lionhead area near West Yellowstone and the mountains around Cooke City:

When the danger is rising, assessing stability is relatively easy. When the danger is decreasing it becomes more difficult especially when the snowpack contains persistent (i.e. long-lasting) layers of faceted snow.  Stability can vary drastically between similar slopes and sometimes across the same slope. This variability has increased during the last week.

This image shows snow water equivalent for the current year (black ), the 30 year average (dashed line) and previous years.  According to the green line for 2007, the snowpack nearly doubled from early Feb to early March.  According to the brown line for 2001, the snowpack increased by 50% starting in late March.  Source: L. Zukiewicz, NRCS

 

 

 

 

Bridger Range, 2012-02-09