Wed, April 03, 2013 Turnagain Pass Avalanche Forecast

Wed, April 3rd, 2013

Alpine

Above 2,500'

2 - Moderate

Treeline

1,000'-2,500'

2 - Moderate

Below Treeline

Below 1,000'

2 - Moderate

0 - No Rating

1 - Low

2 - Moderate

3 - Considerable

4 - High

5 - Extreme


Travel Advice	Generally safe avalanche conditions. Watch for unstable snow on isolated terrain features.	Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern.	Dangerous avalanche conditions. Careful snowpack evaluation, cautious route-finding, and conservative decision-making essential.	Very dangerous avalanche conditions. Travel in avalanche terrain not recommended.	Extraordinarily dangerous avalanche conditions. Avoid all avalanche terrain.
Likelihood of Avalanches	Natural and human-triggered avalanches unlikely.	Natural avalanches unlikely; human-triggered avalanches possible.	Natural avalanches possible; human-triggered avalanches likely.	Natural avalanches likely; human-triggered avalanches very likely.	Natural and human-triggered avalanches certain.
Avalanche Size and Distribution	Small avalanches in isolated areas or extreme terrain.	Small avalanches in specific areas; or large avalanches in isolated areas.	Small avalanches in many areas; or large avalanches in specific areas; or very large avalanches in isolated areas.	Large avalanches in many areas; or very large avalanches in specific areas.	Very large avalanches in many areas.

Avalanche Problem 1

Wet Loose

Wet Loose

Wet Loose avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

More info at Avalanche.org

RECENT ACTIVITY

The most notable avalanche we saw yesterday was off Goat Mountain in the Girdwood valley. We believe a cornice failed due to daytime heating and triggered a slab beneath. This is a common occurrence in this place this time of year. The travel distance of the avalanche was impressive, and farther than I’ve personally seen that path slide.

With continued high daytime temperatures, wet avalanche activity in the afternoon remains the most likely problem to see today. There are numerous examples of this happening over the last few hot sunny days.

Heat induced avalanches are easy to avoid, especially when nighttime temperatures dip below freezing as they are currently. Sometime in the mid afternoon when the snow surface becomes soft or wet, it’s time to avoid south faces, including spending time beneath south faces.

Avalanche Problem 2

Cornice

Cornice

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

More info at Avalanche.org

The cornice problem is really an extension of the heat problem. As the sun bakes the mountains and temperatures rise in the afternoon, unstable features like cornices lose strength and may fail spontaneously.

This problem can be especially dangerous if they trigger larger slabs on the slopes below, as happened on Goat Mountain yesterday.

ADDITIONAL CONCERNS

Even shady aspects have had some avalanche activity since the last major snowfall. Some of these can be attributed to wind slab over loose near-surface-facets. Yesterday we found a low elevation north aspect slab that failed on buried surface hoar in the Placer valley. Everything we’ve seen with this character is breaking at the recent storm snow interfaces ~12-24 inches deep. These are common enough that all steep lines should be treated with a degree of respect.

Weather

Wed, April 3rd, 2013

Yesterday the warm and sunny weather continued. Wind up high reached into the teens and 20s overnight. Overall the only weather factor contributing to avalanche danger was the sun and warm temperatures.

Scattered rain and snow showers are forecasted today with mostly cloudy skies. Temperatures are still expected to reach into the 40s at sea level in the afternoon. If the sun doesn’t shine today there will be less concern for wet avalanche activity on south faces. Wind should be light from the southeast.

Graham will issue the next advisory on Thursday, April 4th.

Observations

Recent Observations for Turnagain Pass

Date	Region	Location	Observer
05/13/24	Turnagain	Observation: Eddie’s, Sunburst, Seattle, Cornbiscuit, Pete’s South	H Thamm
05/13/24	Turnagain	Observation: Turnagain Pass non-motorized side	Amy Holman
05/12/24	Turnagain	Observation: Warm up Bowl	Tony Naciuk
05/07/24	Turnagain	Observation: Turnagain Pass Wet Slabs	A S
04/29/24	Turnagain	Avalanche: Turnagain aerial obs	Tully Hamer
04/27/24	Turnagain	Observation: Johnson Pass	Noah Mery
04/23/24	Turnagain	Observation: Turnagain Sunny Side	Travis SMITH
04/21/24	Turnagain	Observation: Bertha Creek	Anonymous
04/20/24	Turnagain	Avalanche: Spokane Creek	Schauer/ Mailly Forecaster
04/16/24	Turnagain	Observation: Cornbiscuit	Krueger / Matthys Forecaster

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