February 11, 2016

gulmarg avalanche

What does the scale above mean to you as a skier or rider in the Gulmarg backcountry? Read more here.

gulmarg avalanche

Snowpack Discussion

There is greater than 30 cms of new snow at the mid mountain snow study plot in the past 24 hours accompanied with moderate to strong winds in the alpine from a Southerly direction.  Natural avalanches likely, human-triggered avalanches very likely today in the Alpine. Do not tour underneath the large Alpine bowls of Mount Apharwat today. Below Treeline, natural avalanches are possible, and human-triggered avalanches are likely.  Backcountry travel is dangerous today at all elevations and on all aspects.

Choose to ride in groups in the forests of Gulmarg. http://www.deepsnowsafety.org/index.php/. We now have enough snow in the conifer forests above 3200 meters for skiers and riders to get trapped in tree wells. Read more about this phenomenon in the link above. It causes several fatalities each year in other ski regions of the globe.

https://avanet.avatech.com/

See daily snow observations, snow pits, and data from Luke Smithwick and the Gulmarg Ski Patrol. Sign up for a free Avanet account.
See daily snow observations, snow pits, and data from Luke Smithwick and the Gulmarg Ski Patrol. Sign up for a free Avanet account.

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Avalanche Problem #1 – Storm Slab gulmarg avalanchegulmarg avalanche

gulmarg avalanche

Problem Description – Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.

gulmarg avalancheAvalanche Problem #2 – Wind Slabgulmarg avalanche
gulmarg avalanche

 

 

 

 

Problem Description – Release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas.

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Weather Forecast