The Bottom Line: The hazard rating above treeline is MODERATE. Triggering recently developed wind slabs in isolated, steep, leeward terrain is possible. Triggering older and larger Persistent Slabs is becoming less likely but; there is a higher probability the further interior you travel.
Problem 1: Wind Slab
Distribution: Above 2000', leeward to N-E winds. Size: Small. Likelihood: Possible. Sensitivity: Reactive.
Description: On Thursday Feb 14 the winds on Thompson Pass gusted over 70mph. New touchy wind slabs with up to 8" have been observed close to the Pass. No avalanches have been observed; but skiers have reported shooting cracks. Remember that even small avalanches can knock a rider off of or into a terrain trap.
Problem 2: Persistent Slab
Distribution: All aspects above treeline. Size: Large-Very Large. Likelihood: Unlikely. Sensitivity: Stubborn.
Description: There is a widespread buried weak layer (surface hoar) that has 2-4' of slab on top of it. This is a low probability-high consequence setup. There have not been slab avalanches reported since Feb 3, but this weak layer is still WIDESPREAD and deadly. This layer is gaining strength but this REAL problem still lingers. In snowpits, from Crudbuster (mile 40) and northward, this weak layer is failing AND propagating after a lot of force (i.e. ECTP 29) at 45cm down. Evaluate ALL avalanche terrain carefully, choose mellower terrain, AND consciously choose group spacing. If SNOW is the Question, Terrain is the Answer. Now is NOT the time to casually choose large terrain features or objectives.
Problem 3: Glide Avalanches.
There are open cracks from the port to 42 mile between 3500-4000' on multiple aspects. There have been multiple full releases near Girls Mtn and on the Deserted Glacier. It is important to remember glide cracks can release at any time and are not associated with human triggers. New snowfall is covering up these gaping, crevasse-like features so use caution particularly when traveling in FLAT LIGHT. The best way to manage this problem is to limit (AKA avoid) travel underneath and beside them.
The current list of known open glides cracks from West to East:
Since Feb 7 only 2 small skier triggered wind slab avalanches have been reported from the north side of Billy Mitchell - Feb 12. 2x SS-AS-D1 6" crown that 'propagated fairly wide.'
Please share your field observations including signs of stable snow HERE.
The most recent NWS rec Forecast can be found HERE:
336 PM AKST Fri Feb 15 2019
The Thompson Pass Mountain Forecast covers the mountains (above
1000 ft) surrounding Keystone Canyon through Thompson Pass to
Temp at 1000` 5 F 23 F
Temp at 3000` 7-18 F 17-22 F
Chance of precip 0% 80%
(above 1000 FT) 0.00 in 0.14 in
(above 1000 FT) 0 in 2-3 in
Snow level sea level sea level
Wind 3000` ridges NE 8-25 mph E 2-10 mph
SNOWPACK BIG PICTURE: In the top 4' of the snowpack there is a challenging combination of weak layers and new wind slabs in the Valdez region. Below the Jan 23rd buried surface hoar the snow has good strength and structure. The further interior, the problem layers are more widespread and snowpack is considerably shallower.
Recent snowpack history, from top to bottom:
Feb 7-14: Nearly 0" new snow and building north winds (70mph NE gusts on Feb 14 at Thompson Pass.) Widespread surface hoar growth up to 6mm. In windy locations, and close to the pass, most of this surface hoar has been knocked down.
Feb 3-6: 0.7" SWE and 8" of snow from Valdez to Thompson Pass. 8" of new snow was recorded at 5500' on Catcher's Mitt. Freezing level was sea level throughout this cycle.
Jan 30-Feb 1: Natural avalanche cycle on all aspects above 3000', up to size D3. Most ran on buried surface hoar.
Jan 28-30: 2" SWE in Valdez, moderate winds, freezing level 1000'.
Jan 23-25: Multiple days of warm and wet with periods of rain up to 2500'.
Jan 13-22: Mostly clear, cold, and dry with light to moderate north winds. Widespread Surface Hoar growth (up to 15mm) and Near Surface Faceting.
Jan 12-13: 3-10" of new snow with little wind.
Jan 4-12: was VERY cold and dry: moderate winds and wind chill reaching -50F. Pockets of surface hoar and widespread near surface faceting.
Dec 30-Jan 3: The New Year's Eve storm brought nearly 2.5" of SWE to Valdez and almost another 1" (SWE) on the 2-3rd of January. The rain line was 1200' during the Jan 2-3 storm, forming a 1-3" crust locking up all the snow beneath it. These storms accumulated over 3' above 2000' near Thompson Pass. Both of these storms had little wind.
Above 4000' the snowpack averages well over 300cm deep and has good strength and structure (few lemons). Below 4000', the snowpack is significantly shallower and has old problem layers that are bonding well (rounding) and currently dormant: facet-crust combos and BASEL facets (all the way to sea level).
If you get out riding, please send in an observation.
Do a rescue practice with your partners. Always carry a beacon, shovel, and probe, and KNOW HOW TO USE THEM.
Practice good risk management, which means only expose one person at a time to slopes 30 degrees and steeper, make group communication and unanimous decision making a priority, and choose your terrain wisely: eliminating unnecessary exposure and planning out your safe zones and escape routes.
The current hazard rating is MODERATE above treeline. The hazard will rapidly increase as the anticipated 2" of moisture arrives late Saturday.
Both small and large avalanches are possible. There is a lingering Persistent Weak Layer that is MUCH MORE prevalent further north-interior. More info is available by clicking FULL FORECAST below. (All three forecast regions have the same info.)
Please share your field observations HERE.
Forgot your password?
Lost your password? Please enter your email address. You will receive mail with link to set new password.
Back to login