As a popular Tahoe ski resort digs out from a tragedy that killed a skier and buried several others, scientists said predicting how the warming planet will affect avalanches in California is elusive at best.
Just after lifts opened on Wednesday, an avalanche tore through the Palisades Tahoe ski resort, creating a 10-foot-deep debris field that stretched 450 feet long and 150 feet wide. A second avalanche struck in neighboring Alpine Meadows this afternoon, although no one was injured. The U.S. Forest Service and ski resorts take steps to forecast and prevent dangerous slides (PDF), and avalanche fatalities at ski resorts remain rare: Before this week, the last one in California was four years ago.
But what can California’s skiers and snowboarders expect as Sierra Nevada snow patterns become unpredictable due to climate change? Experts say understanding the effects on avalanches is tricky: Climate change is not just a matter of warming temperatures but also altered patterns in storms and snow cover.
An array of factors such as wind, rain, previous snowpack and temperatures can all enter into the equation of what causes a mass of snow to slide down a mountain.
“We are humans working in a natural world. And so everybody does the best they can,” said Jim Steenburgh, a University of Utah professor of atmospheric sciences and author of the book Secrets of the Greatest Snow on Earth.
The circumstances that lead to avalanches are multifaceted, Steenburgh said: a weak layer in the snowpack, a steep slope and a trigger — usually people on the slope. The frequency of human-triggered avalanches in the future will largely depend on how many skiers and snowboarders recreate in risky backcountry areas.
That also means untangling the effects of climate change is especially difficult, or “elusive,” as one team of scientists said.


