Valdez
Above 3,000ftConsiderable
1,500 to 3,000ftConsiderable
Below 1,500ftConsiderable
Degrees of Avalanche Danger
Avalanche Problems
Problem 1
Arctic air and strong to very strong northeast winds will set in over the next 48 hours. Moderate winds on 12/10 have already begun to build slabs on lee aspects. Winds will intensify and strip into deeper layers of our snowpack creating deeper slabs. Expect to find fresh wind slabs 1-2 feet in depth that are reactive to human triggers. Wind slab avalanches will have the potential to step down into deeper faceted layers in our snowpack, (see problem 1) and produce larger avalanches. Avoid recently wind loaded slopes in terrain steeper than 32°. The hazard for this avalanche problem will be increasing over the next 48 hours.
Likelihood:
- Almost Certain
- Very Likely
- Likely
- Possible
- Unlikely
Size:
- Historic
- Very Large
- Large
- Small
Trend
- Increasing
- Steady
- Decreasing
Problem 2
There is a 2-3 foot deep slab sitting on the November facets. The depth of this slab increased a bit the night of 12/9 with 6 inches of snow in Valdez, 3-4 inches on Thompson Pass and 10 inches at 46 mile. Northeast wind are forecasted to increase over the next 48 hours moving from moderate to very strong. Both of these changes in weather will make triggering a persistent slab avalanche more likely. It is possible that we will see some natural avalanche activity on southerly aspects in the next 48 hours.
On 12/8 a remote triggered/sympathetic avalanche event (see observation section) is a clear sign that our persistent slab avalanche problem is hanging on by its fingernails. This is especially true in wind sheltered areas. In locations were old wind slabs exist above the November facets, weak layers may be more stubborn to triggers. But the same weak layer exists and dangerous human triggered avalanches are possible in these locations as well.
The 24 hour rule will not apply for our current setup. The only successful mitigation practices for a persistent slab avalanche problem are patience, and a conservative approach in choosing terrain. Good protocols are very important as well during this type of avalanche problem ie: only exposing one person at a time to an avalanche prone slope, good communication and having an escape route should a slope fail.
Some important things to remember about a persistent weak layer problem is that tracks are not a sign of stability. A slope can fail after many tracks have been laid down. Remotely triggered avalanches are possible (triggering a slope above, below or adjacent to your position). Pay attention to the terrain above you and what the consequences would be if that slope were to fail.
Photo of Remote triggered/sympathetic avalanches on 12/8
1cm+ chained facet found buried 40 cms (16″) on Catchers Mitt 3500′ SE aspect.
Likelihood:
- Almost Certain
- Very Likely
- Likely
- Possible
- Unlikely
Size:
- Historic
- Very Large
- Large
- Small
Trend
- Increasing
- Steady
- Decreasing
Avalanche Activity
12/8- Large remote trigger/ sympathetic avalanche event occurred 12/8 with avalanches extending from Gully 1 to Nicks. Avalanches were soft slabs that ranged in size from D1-D3. Over 10 separate avalanches were counted with crown depths averaging 2-3′. One avalanche had a crown length of half a mile while another was triggered over a mile away from the point of collapse. See observation section for full report and more photos.
12/7- Only a few natural avalanches were noted during the last storm. It is likely there were more during the storm, but crowns may have been filled in by subsequent wind and snow.
D2’s on Town mountain was observed ~3000′
A couple of D2’s were noted in N. Oddessey gully and Big Oddessey.
D2 on 40.5 mile peak ~5500′.
12/2-12/3- Several natural D2 avalanches were noted on south aspects of Three pigs, Hippie Ridge and Averys. These windslab avalanches originated between 4000-5500 feet elevation.
Weather
NWS Watches and Warnings
Northeast Prince William Sound-
Including the cities of Valdez and Thompson Pass
506 AM AKST Sat Dec 11 2021
...HIGH WIND WARNING IN EFFECT FROM 3 PM THIS AFTERNOON TO 9 AM
AKST MONDAY THROUGH THOMPSON PASS...
* WHAT...Northeast winds 30 to 50 mph with gusts up to 75 mph
expected.
* WHERE...Thompson Pass.
* WHEN...From 3 PM this afternoon to 9 AM AKST Monday.
Point forecast for Thompson Pass
Detailed forecast for Thompson Pass (mid elevation 2000-4000′)
DATE SATURDAY 12/11 SUNDAY 12/12
TIME (LT) 06 12 18 00 06 12 18 00 06
CLOUD COVER OV OV OV BK SC FW FW CL FW
CLOUD COVER (%) 70 70 70 65 30 15 5 5 15
TEMPERATURE 12 4 1 -3 -6 -8 -9 -10 -12
MAX/MIN TEMP 13 -7 -3 -13
WIND DIR NE NE NE NE NE NE N NE NE
WIND (MPH) 27 28 32 34 34 35 36 31 25
WIND GUST (MPH) 74 74 77 77 75 74 73 73
PRECIP PROB (%) 10 10 5 5 0 0 0 0 5
PRECIP TYPE
12 HOUR QPF 0.00 0.00 0.00 0.00
12 HOUR SNOW 0.0 0.0 0.0 0.0
SNOW LEVEL (KFT)0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
Snow and Temperature Measurements
| Date: 12/11 | 24 hr snow | HN24W* | High Temp | Low Temp | Weekly SWE (Monday- Sunday) | December Snowfall | Season Snowfall | HS (Snowpack depth) |
| Valdez | 0 | 0 | 30 | 16 | 1.58 | 46 | 70 | 29 |
| Thompson Pass | ~3-4 | N/O | 17 | 8 | N/O | ~30 | 149 | N/O |
| 46 Mile | Trace | 0 | 20 | 11 | .9 | 22 | 22** | 24
|
All snowfall measurements are expressed in inches and temperature in Fahrenheit. 24 hour sample period is from 6am-6am.
* 24 hour snow water equivalent/ SWE.
** Season total snowfall measurements for 46 mile began December 1st.
Season history graphs for Thompson Pass
Click on links below to see a clear and expanded view of above Season history graphs
Additional Information
Winter weather began early this season, with valley locations receiving their first snowfall on the last day of Summer (September 21st). Following this storm, above average temperatures and wet weather occurred from late September through early November. During this time period Thompson Pass received 96 inches of snowfall by November 7th and Valdez recorded 7.73″ of rain.
After the 7th of November our region experienced a sharp weather pattern change. Temperatures dropped below seasonal norms and snowfall became infrequent. Between the time frame of November 7th- November 28th Thompson Pass only reported 19″ of snow with 1.1″ of Snow water equivalent (SWE). Temperatures remained below 0° F for most of the period. This cold/dry weather caused significant faceting of the snowpack, with poor structure the result.
Moderate snowfall returned to our area the last day of November and deposited 6-12 inches of new snow. The amount varied depending upon the locations’ proximity to the coast. As the storm exited on the 2nd of December it was quickly replaced by moderate to strong northeast winds.
On 12/5-12/6 Valdez received 2 feet of new snow with Thompson Pass reporting 16″. Blaring red flags like collapsing, shooting cracks and propagation in stability tests were immediately present. On 12/8 a significant remote/ sympathetic avalanche event occurred from Gully 1 through Nick’s Happy Valley. Incremental loading has resulted in a dangerous persistent avalanche problem at the present.
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