Sat, April 11, 2015 Turnagain Pass Avalanche Forecast

Sat, April 11th, 2015

Alpine
Above 2,500'

Moderate (2)

Treeline
1,000'-2,500'

Moderate (2)

Below Treeline
Below 1,000'

No Rating (0)

Alpine Above 2,500'		Moderate (2)
Treeline 1,000'-2,500'		Moderate (2)
Below Treeline Below 1,000'		No Rating (0)

Danger Scale:

No Rating (0)

Low (1)

Moderate (2)

Considerable (3)

High (4)

Extreme (5)

Avalanche Problem 1

Persistent Slabs

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

More info at Avalanche.org

A storm that deposited 2 feet of snow in the higher elevations 2 days ago has left slabs that are generally well bonded to underlying surfaces. While this bonding has been good in recent tests, we saw natural slab activity after the storm had subsided. Yesterday this occurred mainly on steep slopes that were receiving direct sun. More of the same can be anticipated today. Factors that will increase the likelihood of triggering will be slopes over 35º and approaching 40º, heating from direct sunlight and large triggers such as groups.

We have limited data from North facing terrain. As such it will be important keep slope angles 35 or lower if you find yourself on terrain facing the North half of the compass.

Natural slab activity on Seattle Ridge on steep sunlit slopes observed yesterday, April 10th.

2′ Slab with a close up of the crown. Starting zone ~2,300′ SE aspect

Slab post storm Seattle 4-10-15

A view of the debris of the avalanche pictured above. Avalanche ran ~1,000′ vertical.

debris

Avalanche Problem 2

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

Both wet loose and wet slab activity can be expected on steep sunlit slopes. In the higher elevations, sun will impact slopes and “grease” the interfaces between the slab and bed surfaces. Those bed surfaces are crusts on East, South and West aspects.
In the lower elevations, a warm and weak snowpack will allow for the chance of medium to high volume wet loose avalanches during the heat of the day. Volume will be dictated by terrain; more sustained steep slopes will produce more debris.
Pay attention to the temps and sun today. Dial back your slope angles if and when you notice rollerballs, wet loose avalanches or the snow surface becomes damp and sloppy…

…or when you sink into your waist after stepping out of your skis or board:

Additional Concern

Deep Persistent Slabs

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.

More info at Avalanche.org

Weak layers of faceted snow buried as deep as 5’ sit on some slopes on North facing terrain in the Alpine. This set up will not be found everywhere. Because of this variability, it is especially important to treat this terrain with suspicion. Assessment of this issue is very difficult. The best strategy for “managing” this problem is to avoid this terrain for the time being and give those underlying weak layers ample time to adjust to the large loads (3’+ snow/3”+ H20 over the last week) that have been placed on them. This is a low likelihood/high consequence scenario that requires patience and time.

Weather

Sat, April 11th, 2015

The last 24 hours has seen the beginning of a slow and gradual exit of a large low pressure system from our area. That system is in fact still circulating around the Gulf of Alaska. Precipitation, winds, and temps have all diminished. Just a trace of snow fell in the morning hours yesterday. Winds have slowed and temps have cooled slightly overnight.

Today expect showery conditions, with occasional clouds and mostly sunny skies as that system continues to weaken and spin slowly around the Gulf. Temperatures at 1,000′ will climb into the mid 30s F. Winds will be calm and just a trace of precipitation will fall. Snow showers could produce greater amounts in some areas.

The extended outlook is showing a continuation of this pattern over the next several days, as we remain under the influence of broad and weak circulation around the Gulf.

PRECIPITATION 24-hour data (6am – 6am)

	Temp Avg (F)	Snow (in)	Water (in)	Snow Depth (in)
Center Ridge (1880′)	30	trace	.1	72
Summit Lake (1400′)	29	0	0	12
Alyeska Mid (1700′)	32	trace	0	42

RIDGETOP 24-hour data (6am – 6am)

	Temp Avg (F)	Wind Dir	Wind Avg (mph)	Wind Gust (mph)
Sunburst (3812′)	22	ENE	7	24
Seattle Ridge (2400′)	26	sensor	is	rimed

Observations

Recent Observations for Turnagain Pass

Date	Region	Location	Observer
05/22/23	Turnagain	Avalanche: Tincan	Nick D'Alessio
05/12/23	Turnagain	Avalanche: Tincan, Sunburst, Magnum, Cornbiscuit	Heather Thamm
05/07/23	Turnagain	Observation: Tincan – Bear Tracks	CNFAIC Staff
05/05/23	Turnagain	Observation: Seattle Ridge	AS/ WW Forecaster
05/02/23	Turnagain	Observation: Cornbiscuit	Schauer/ Sturgess Forecaster
05/02/23	Turnagain	Observation: Seward Hwy Turnagain Pass	Joel Curtis
04/30/23	Turnagain	Observation: Magnum	Ayla, Kit Crosby, Barton
04/29/23	Turnagain	Observation: Tincan	John Sykes
04/28/23	Turnagain	Avalanche: Taylor Pass/Pastoral	Schauer/ Creighton Forecaster
04/28/23	Turnagain	Avalanche: Tincan	Andy Moderow

Riding Areas

Updated Mon, May 15th, 2023

Status of riding areas across the Chugach NF is managed by the Glacier and Seward Ranger Districts, not avalanche center staff. Riding area information is posted as a public service to our users and updated based on snow depth and snow density to prevent resource damage at trailhead locations. Riding area questions contact: mailroom_r10_chugach@fs.fed.us

Area	Status	Weather & Riding Conditions
Glacier District
Johnson Pass	Closed	Closed May 15.
Placer River	Closed	Closed May 15.
Skookum Drainage	Closed	Will close to motorized use on April 1, 2023 per the National Forest Plan.
Turnagain Pass	Open	Chugach NF staff will be assessing daily after May 15th. Please keep machines on the snow and avoid brown spots to keep this area open as long as possible.
Twentymile	Closed	Scheduled closure May 1.
Seward District
Carter Lake	Closed	Scheduled closure May 1.
Lost Lake Trail	Closed	Scheduled closure May 1.
Primrose Trail	Closed	Scheduled closure May 1.
Resurrection Pass Trail	Closed	Closed to motorized use for the 2022/23 winter season per Forest Plan. Open next season.
Snug Harbor	Closed	Extended opening until May 15.
South Fork Snow River Corridor	Closed	Scheduled closure May 1.
Summit Lake	Closed	Scheduled closure May 1.