Haines Avalanche Center

Forecast as of 2019-01-21 at 12:00 pm and expires on 2019-01-22

Above 2,500ftModerate

1,500 to 2,500ftLow

Below 1,500ftLow

Degrees of Avalanche Danger

Avalanche Problems

Problem Details

The last storm cycle ended January 1st. It featured strong SE winds, and 1-2.5" of SWE. It rained up to about 4000ft for a few hours at the end of the storm. We've been in deep freeze with arctic outflow (NW winds) ever since.

Problem #1: Wind Slab:

Location: Specific slopes in the alpine above 2,000ft, where north/NW winds the last three weeks caused wind loading on lee aspects beneath ridgelines and terrain features. Recent reports found areas of wind slab (3-8" thick) that are poorly bonded and easy to trigger. Be sure to dig around in high-alpine areas to assess for yourself how well-bonded the upper snowpack is. Variability will be high, so evaluate each slope carefully. Hand pits and slopes tests will be helpful in mapping out this potential danger. In large or steep terrain, slabs as thin a few inches can sweep you into dangerous situations. 

January 8th Snow pit from the Lutak zone, at 2700ft, N aspect. Notice fresh wind slabs in top 15cm (easy triggering), and hard triggering down 35cm.

Problem #2: Deep Slab:

Location: Chilkat Pass Zone, all aspects above 3,500ft. Avalanche Size: Large. Likelihood of Triggering: Possible.

We've had mixed reports of lingering weakness in an old facet layer about 80-100cm deep (more like 45cm deep in shallower areas near Nadahini). These 2mm facets are sitting over a slick rain crust, and have produced isolated deep avalanches during storms over the last few weeks. In some areas (mainly lower elevations with deeper snowpack) this layer is not reactive, but we did get one report of easy triggering on this deep weak layer in snowpit tests from the north slopes of Mineral Mountain on January 3rd, and another from Nadahini area on Jan 20th. The most likely way to trigger this layer will be from areas of thin snowpack, near rocks and ridgelines. Heavy triggers such as snowmachines, cornices, or hard cliff drops increase the odds of collapsing this weak layer. Remote triggering will be possible, so careful group management and wide spacing is essential. The best way to manage this danger is to plan for the unpredictable, and know where your safe zones are. Consider the consequences of a slab this deep ripping out before you commit to avalanche terrain.

Above: Nadahini snow pit from 20-Jan-2019


Above: Deep slab avalanche in the Chilkat Pass zone from early January. NE aspect near 5000ft.


Light snow on Monday will taper off by evening. Around 3" fell in the Lutak zone. Tuesday should feature some clearing and a break in the weather before a major pattern change. Wednesday-on we will have increasing south winds, rapidly warming temperatures, and rising snow levels with periods of heavy precipitation. It's hard to pin down the details but 1-2" of precipitation is likely by Friday, with snow levels peaking around 3000ft.

   Snow Depth [in] Last 24-hr Snow/SWE [in] Last 3-days Snow/SWE [in]  Today's Freezing Level [ft]  Today's Winds Next 24-hr Snow/SWE
Mount Ripinsky @ treeline
 43" 3" / 0.15  3" / 0.15  0 mod, N 0" / 0.00    *
Flower Mountain @ treeline
 40" 1" / 0.05  1" / 0.05  0 mod, NW 0" / 0.00     *
Chilkat Pass @ 3,100ft
 28" 1" / 0.05  1" / 0.05  0 lmod, NW 0" / 0.00   *

( *star means meteorological estimate )

Additional Information

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.