4/18: Numerous moderate to very large wet loose avalanches were seen and reported on south aspects from sea level up to 6000′.
4/17: Full depth wet slab avalanches were observed on south faces of Town Mountain, Hogsback and Hippie Ridge.
4/16: Widespread wet loose avalanches observed in the Port of Valdez up to 5000′ on east through west aspects.
A soft slab avalanche was observed on Hogsback that initiated from a rockband at ~4500′, west aspect, ~500′ wide. Looked to be about 2-3′ deep, but was observed through binoculars so that is just a guess. Avalanche may have been snowmachine triggered as there were tracks directly adjacent to the avalanche, but that is unconfirmed.
4/14: Observed numerous small to moderate wet loose slides off solar aspects up to 4000′.
4/6: Small to moderate dry loose “sluffs” were observed on east through northwest aspects above 3000′ in terrain steeper than 40°. Did not observe any soft slab avalanches triggered by dry loose slides.
3/26: Small natural wet slab avalanche that originated from a point release was observed at MP 40 on a south aspect. 100′ wide, originating from ~2000′, ran to ground.
3/22: Small snowboard triggered wind slab avalanche reported in skate park. ~3000′, southeast aspect, 1 foot deep, ~40′ wide. SS-ARu-R1-D1.5-I. Other small natural releases were reported in the area as well.
3/14: Numerous D1 wet loose avalanches observed 3/14 on south aspects in steep terrain.
3/11: 2 Human triggered avalanches observed on the Thompson Pass corridor.
Skier triggered avalanche in Nicks Happy Valley. Skier was traversing the wind loaded northwest aspect of the gully and released a slab ~1 foot deep and 100′ wide, ran ~150 vertical feet to the bottom of the gully. SS-ASu-D1.5-I.
3/5: -Natural D 2.5 occurred on the NW aspect shoulder of the Python Buttress “Ptarmigan Drop” milepost 31. Avalanche crown was reported to be 10-15 feet deep by DOT and ran to the ground. Crown was quickly filled back in by intense snow transport.
3/4: A natural D3 avalanche ran above the 37 mile tsaina bridge. South aspect ~5500′, stepped down multiple times, ran to the ground in places. The main debris fell short of the highway, mature uprooted trees 6-12 inches in diameter were thrown onto the road by powder blast.
-The gully downstream of Bridal Veil Falls produced a large avalanche, D2.5, that buried the river with over 10′ of debris, the powder blast pushed sticks into the parking lot on the other side of the road.
3/3: DOT mitigation work produced another large avalanche that affected the Richardson Highway at ~ mile 39. Initial reports stated that the avalanche buried the highway under 15 feet of debris for ~500 feet.
2/28: Natural wind slab avalanche 4000′. N-HS-R2-D2, West aspect slope that descends from Crudbuster basin into IguanaBacks. Stepped down immediately below initial crown, to the ground in places.
2/26: Large natural observed at 48 mile off Point 5064 (Stuart). N-HS-R3-D3, N-W aspects. Observed from the highway. Looked fresh, probably within the last 24 hours. Appears to have released from a N aspect bowl ~40-45° at~4500′, then stepped down and wrapped around the corner onto NW-W aspects. Crown on step down is estimated to be over 3 meters deep in places. Couldn’t see extent of track length. Crown was over 1/2 mile wide. 3 small, sympathetic pockets were observed over 1/2 mile away in moderate terrain with crowns ~1-2 meters. Picture taken from over 3 miles away.
2/24: Natural avalanche observed on the north face of Goodwills’ ~5500′, D-2.5, 200-300′ wide. Ran to the bottom of the slope ~600′, crown ~5′ deep.
2/23: – Natural avalanches D2-2.5 on the east face of Mt. Tiekel were observed.
2/21: Multiple natural and human triggered avalanches were observed 2/21.
Debris along the highway after DOT cleanup work.
Debris that over ran the highway and was deposited into the Tsaina Gorge.
Natural near the toe of the Worthington Glacier.
2/20: Two side by side avalanches were observed on the NW shoulder of the Python buttress ~3500′. Crown 2-300′ across and ~3’+ deep. These slides ran into the flat ~800 vertical feet. Slides were triggered by DOT mitigation work 2/19.
2/20: 2 paths on Three Pigs at MP 42 slid naturally to the middle to lower portion of their aprons, D2.5. Low clouds prevented ability to see what elevation they originated from.
2/20: A natural avalanche was reported on the north shoulder of Mt Tiekel at ~4500′. Details were limited but the entire slope avalanched and crown was reported to be 2 meters deep. R5-D2.5~.
2/19: A natural avalanche at 32 mile buried the Richardson Highway under 10 feet of snow for ~100′. This caused the highway to close for the majority of the day. This slide released from the lower bench of RFS on a north aspect.
2/14: Dry loose D1-2 natural avalanches were observed running over the Wowie Zowie ice climb in Mineral Creek.
2/13: Natural and human triggered D1 avalanches were observed in Keystone Canyon.
2/12: A D3 avalanche at MP 38 hit the Richardson Highway and closed the road. Released on a south aspect in the upper elevation start zones, ~5500′, and stepped down around 4-4500′. Further DOT mitigation efforts on Three Pigs and 40.5 Mile produced no results.
4/23: Southerly flow will push clouds and moisture into our area. Around .25 inches of water is forecasted with freezing line hovering around 2000′. This could translate into a few inches of heavy snow for the top of Thompson Pass at the road.
The Thompson Pass Mountain Forecast covers the mountains (above
1000 ft) surrounding Keystone Canyon through Thompson Pass to
This forecast is for use in snow safety activities and emergency
Temp at 1000` 46 F 34 F
Temp at 3000` 32 F 30 F
Chance of precip 70% 80%
(above 1000 FT) 0.09 in 0.21 in
(above 1000 FT) 0-2 in 0-4 in
Snow level 2200 ft 2100 ft
Wind 3000` ridges SW 3-8 mph SW 3-8 mph
Thompson Pass “DOT”
HN24W= total water received last 24 hours in inches
Thompson Pass weather history 19/20 season beginning 12/21. Click on links below to see full size image.
TP DEC 19
TP Jan 2020
TP WX chart February 2020
TP wx chart March 2020
TP wx chart through 4/13
The spring shed cycle is here. Pay attention to what the sun is doing to the slope you are traveling on, and what is above you. The change in seasons has been especially drastic this year which can make the mountains react in unpredictable ways, and produce large avalanches in areas that don’t normally see them.
Faceted snow still exists at the base of our snowpack in Intermountain and Continental locations. This faceted snow was created by the dry, brutal cold temperatures in January. It is possible that we will see these layers re-activate in Continental locations when heat penetrates down to these deep layers.
Our area has encountered the first part of our Spring shed, caused by temperatures remaining above freezing at elevation without overnight refreezes. A lot of snow has fallen off the mountains which has relieved a lot of stress from our transitioning snowpack. On 4/21 temperatures began to fall below freezing at Thompson Pass and above, which will allow natural avalanche activity to slow down for the time being. The spring shed will continue once skies clear and the sun begins to create large diurnal temperature swings during the day, or if our area receives significant rain on snow.
Forecast Confidence is Moderate.
Resolution is Moderate.
If you see something in the mountains that could contribute to this forecast, leave a public observation. The more observations we receive, the better we can tune our forecast. If you would rather not post an observation publicly, feel free to send me an email at [email protected]
Send in your best mountain recreation photos to [email protected] so we can post a photo of the week!
Photo of the Week
The avalanche hazard is considerable at low elevations and moderate at mid and upper elevations. The snowpack is isothermal at low elevations, which will make triggering wet loose avalanches likely on all aspects, and wet slab avalanches possible on southeast through southwest aspects at low elevations. At mid and upper elevations the hazard is moderate. Temperatures have dipped below freezing at Thompson Pass and above, this has allowed the surface snow to gain strength by forming a crust. Triggering wet loose or wet slab avalanches is still possible on terrain steeper than 30° once temperatures warm up through the day and surface snow becomes moist.
Forgot your password?
Lost your password? Please enter your email address. You will receive mail with link to set new password.
Back to login
Enter the destination URL
Or link to existing content