What does the scale above mean to you as a skier or rider in the Gulmarg backcountry? Read more here.
Snowpack Discussion
Avalanche danger above 3000 meters is Moderate. Natural avalanches are unlikely, human-triggered avalanches are possible. Below 3000 meters the avalanche danger is Low. Natural and human triggered avalanches are not likely.
The avalanche problems for today are Wind Slabs and Deep Slabs. Wind slabs exist beneath ridgelines and ridgetops in the Gulmarg backcountry. These slabs are stiff and difficult to trigger, however if you found the right spot, can be triggered. Choose your terrain wisely and consider the consequences if you were caught and carried over the terrain that is in front of you and beneath you.
In the middle of our snowpack, there is a weak buried crust. Two days ago, all of the snow on top of this crust avalanched in South Apharwat bowl naturally. This is “class 1” data, telling you that this layer is now “switched on” and ready to avalanche with a skier or rider finding the right trigger point. The most likely trigger point is near rocks and shallow areas of the snowpack (near ridgelines). The most likely time of day for this to happen will be between 12-3 pm.
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.
—————————-
Avalanche Problem #1 – Deep Slab
Problem Description – Release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer, deep in the snowpack or near the ground. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage. They commonly develop when Persistent Slabs become more deeply buried over time.
Deep Persistent Slabs are destructive and deadly events that can take months to stabilize. You can trigger them from well down in the avalanche path, and after dozens of tracks have crossed the slope.
Avalanche 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)
Gulmarg Ski Area (green zone) Timings for 22/2/2016:
Phase 1 – 0830 – 1630 (last cabin at 1630)
Phase 2 – 0900 – 1600 (last cabin 1530)
Chair Lift – 0900 – 1530 (last chair 1500)
Beacon Training Center on Merry Shoulder is OPEN with 2 BEACONS. Beacon Training Center in Gulmarg meadow across from Hotel Hilltop is OPEN with 1 BEACON. Come by Gulmarg ski patrol base at mid mountain to learn the location of the beacon training area on Merry Shoulder and hone your search skills and times.
Next avalanche talk is Wednesday 24 February, 2016 at 7:30pm at Hotel Hilltop. Hotel Hilltop is located across from the ice skating rink in Gulmarg meadow. Talks will continue every Wednesday night at 7:30 pm through 30 March, 2016.