February 19, 2016

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

gulmarg avalanche

Snowpack Discussion

Overall avalanche danger rating above 3000 meters is Moderate.  Natural avalanches not likely, human-triggered avalanches possible. Small wet loose avalanches can potentially be triggered on East to Southeast facing aspects between the hours of 12 pm – 3pm today.  The danger here isn’t the avalanches themselves, but the terrain traps you could be carried over if you were caught in one (rocks). Choose terrain wisely to avoid this avalanche problem. Regarding Wind Slabs at ridge tops, they appear to be confined to lee aspects near the top of Mount Apharwat, and should be expected on similar aspects and elevations further afield. Once again, fairly small avalanches, but if you triggered one in steep terrain with rocks and cliffs underneath, it could cause injury if you were carried over this terrain. As always, choose your terrain wisely today. Avalanche danger below 3000m is Low. Natural avalanches unlikely, human triggered avalanches unlikely.

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.

—————————-

Avalanche Problem #1 – Wet Loose

loose-wet

Problem Description –

Release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. They generally move slowly, but can contain enough mass to cause significant damage to trees, cars or buildings. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

Travel when the snow surface is colder and stronger. Plan your trips to avoid crossing on or under very steep slopes in the afternoon. Move to colder, shadier slopes once the snow surface turns slushly. Avoid steep, sunlit slopes above terrain traps, cliffs areas and long sustained steep pitches.

gulmarg avalancheAvalanche Problem #2 – Wind Slab

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.

—————————
Weather Forecast (link:http://www.snow-forecast.com/resorts/Gulmarg/6day/mid)