16 February, 2017

What does the scale above mean to you as a skier or snowboarder in the Gulmarg backcountry? Remember, this advisory is for the Gulmarg backcountry, which means the terrain that is outside of Gulmarg Ski Area. The red areas in the photo below are the Gulmarg backcountry, and the green area is Gulmarg Ski Area. This advisory does not apply to the green zone ski area. Read more here.

For ski area updates during the day please join Gulmarg Avalanche Conditions page on Facebook: http://bit.ly/2jowwOM.

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Snowpack Discussion
16 February 2017 – Avalanche danger above 3000 meters is Moderate (2) today. Natural avalanches unlikely, human triggered avalanches possible.  Old Wind Slabs on cold Northwest to Northeast aspects  in mid-slope isolated terrain features still exist.  They are small in size and are still possible to be triggered. Dry Loose avalanches can be expected to be triggered on all aspects above 3000 meters on steep terrain today, especially with diurnal warming.

http://www.deepsnowsafety.org/index.php/. We now have enough snow in the conifer forests 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.

http://mountainhub.com/

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See daily snow observations, snow pits, and data from the Gulmarg Avalanche Advisory. Sign up for a free Mountain Hub account.

Avalanche Problem #1 – Wind Slab

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.

Wind slab instability persists in the Gulmarg backcountry.  This is a North facing panel mid slope, and it is isolated from the rest of the terrain in the area. With a ski cut a small size 0.5 wind slab Avalanche propagated.  Class 1 data of isolated instability in the Gulmarg backcountry on Northerly aspects below ridgelines and in mid-slope isolated terrain features. gulmarg-avalanche-advisory.com.

Gulmarg Ski Area (green zone) Timings for 15/2/2017:

Phase 1 – 8:15am – 4:30 pm (last cabin at 4:15pm)
Phase 2 – 8:45am – 4:00 pm (last cabin at 3:45pm)*
Chair Lift – 8:45am – 4:00 pm (last chair at 3:45pm)

*If we lose visibility or have strong winds at the top station today the second phase of the gondola will need to be closed.

Beacon TrainingToday there are (1) beacons buried on Merry Shoulder today.  The beacon training area here in Gulmarg is located on Merry Shoulder. The orange dot (see photo below) indicates where a red flag is next to a large birch tree. This is the “point last seen”. Start your search here. We have one, two, and three beacons buried here daily.  Please do not dig up the beacons, simply cycle through your Primary (signal) search, Secondary (flux line) search, Pinpoint search, and then Probing. A probe strike indicates the end of your search. If you’re interested in learning more, please come by Gulmarg Ski Patrol base at the bottom of the chair lift.

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Next avalanche talk is Tuesday, 21 February 2017 at 7:30pm at Pine Palace Resort. Pine Palace Resort is located in Gulmarg meadow. Talks will continue every Tuesday night at 7:30 pm through 28 March, 2017.