Tue, December 04, 2018 Turnagain Pass Avalanche Forecast

Tue, December 4th, 2018

Alpine
Above 2,500'

Moderate (2)

Treeline
1,000'-2,500'

Low (1)

Below Treeline
Below 1,000'

No Rating (0)

Alpine Above 2,500'		Moderate (2)
Treeline 1,000'-2,500'		Low (1)
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

Wind Slabs
Almost Certain

Very Likely

Likely

Possible

Unlikely

Likelihood
Historic

Very Large

Large

Small

Size

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Likelihood of Avalanches

This graphic depicts how likely you are to trigger avalanches or encounter natural avalanches while traveling on avalanche prone slopes. Unlikely means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. The chance of triggering or observing avalanches increases as we move up the scale. Certain means that humans will be able to trigger avalanches on many slopes, and natural avalanches should be expected.

Size of Avalanches

This graphic depicts the potential size and destructive force of expected avalanches. Small avalanches are not large enough to bury humans and are relatively harmless unless they carry people over cliffs or through trees or rocks. Moving up the scale, avalanches become large enough to bury, injure, or kill people, large enough to bury or destroy vehicles and break a few trees, and large enough to destroy railway cars, buildings, or a substantial amount of forest. Historic avalanches are massive events capable of destroying villages and gouging or altering the landscape.

More info at Avalanche.org

Be on the lookout for wind slabs in steep unsupported terrain. Strong easterly winds on Saturday afternoon loaded leeward slopes in the Alpine. Surface conditions at upper elevations yesterday varied from wind skin to rime crust to sastrugi to wind slab. Winds are forecast to increase again today and there is still snow available for transport. Look for stiff, pillowed snow and cracking and listen for hollow, drum-like sounds. Loading patterns can be very localized and it is crucial to look for clues indicating where the snow is being distributed.

Sunburst weather station wind profile from Friday afternoon to Tuesday morning

Surface conditions on Sunburst and cross-loading on the north side of Magnum, December 3, 2018. Photo: Heather Thamm

Avalanche Problem 2

Persistent Slabs
Almost Certain

Very Likely

Likely

Possible

Unlikely

Likelihood
Historic

Very Large

Large

Small

Size

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.

Likelihood of Avalanches

Size of Avalanches

More info at Avalanche.org

In the Alpine, sitting anywhere from 1 to 3′ below the snow surface, is a thin layer of weak snow (buried surface hoar/BSH). It got a good shake on Friday during the earthquake and a number of quake triggered avalanches are thought to have run on this BSH (buried November 23rd) layer. Did that shake it up enough??? That is the hard to answer question. An observer Sunday found this layer to still be reactive in a snowpit on Sunburst right around 2500′. Yesterday at 3100′ on Sunburst there were no results testing this layer but it was very easy to spot laid over in the snowpack. The concern is finding a slope with buried surface hoar that is still intact, reactive and that propagates into an avalanche. At this point obvious signs of instability may not be observed but some lingering suspicion is advised even as the likelihood decreases. As always use safe travel protocol and choose terrain with consequences in mind i.e. where is the avalanche path and where would I end up if the slope slides?

Weather

Tue, December 4th, 2018

Yesterday: Skies were partly sunny with temperatures in the low 30Fs to mid 20Fs. Winds were easterly 5-15 mph with gusts in the 30s. Overnight temperatures dropped into the mid 20Fs to high teens.

Today: The forecast is for mostly cloudy skies with a chance of rain/snow showers with rain/snow line around 800′. Temperatures will be in the mid 30Fs to mid 20Fs depending on elevation. Winds are forecast to be easterly 20-40 mph with gusts into the 50s.

Tomorrow: Cloudy skies and rain/snow showers are forecast to continue. Winds should decrease and temperatures will be slightly warmer. The National Weather Service long term discussion had a couple of interesting quotes this morning, “A high degree of uncertainty will make for an interesting forecast for the end of the week and into early next week. In short it looks like an active and wet period, but the details are murky due to model disagreement and inconsistency being far below normal.”

*Seattle Ridge wind sensor is rimed over. Alyeska Mid Wx Station and Summit Lake Snotel snow depth sensor are not functioning.

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

	Temp Avg (F)	Snow (in)	Water (in)	Snow Depth (in)
Center Ridge (1880′)	27	0	0	13
Summit Lake (1400′)	17	0	0	*no data
Alyeska Mid (1700′)	28	0	0	*no data

RIDGETOP 24-hour data (6am – 6am)

	Temp Avg (F)	Wind Dir	Wind Avg (mph)	Wind Gust (mph)
Sunburst (3812′)	20	E	8	30
Seattle Ridge (2400′)	25	*no data	*no data	*no data

Observations

Recent Observations for Turnagain Pass

Date	Region	Location	Observer
12/06/19	Turnagain	Avalanche: Sunburst	Billy Finley
12/04/19	Turnagain	Observation: Sunburst	A.Johnston-Bloom/ W.Wagner/ R.Van Luit Forecaster
12/03/19	Turnagain	Observation: Hippy Bowl	Nick Langowski
12/01/19	Turnagain	Observation: Tincan, All elevations	Eric Roberts
12/01/19	Turnagain	Observation: Tincan	Andy Moderow
11/30/19	Turnagain	Observation: Tincan Treeline Plateau/ Common Bowl/ Ridge	Eric Roberts
11/29/19	Turnagain	Observation: Sunburst Ob #2	Aleph Johnston-Bloom Forecaster
11/29/19	Turnagain	Observation: Sunburst Ob #1	Aleph Johnston-Bloom Forecaster
11/27/19	Turnagain	Observation: Tincan	Aleph Johnston-Bloom Forecaster
11/25/19	Turnagain	Observation: Sunnyside	Graham Predeger Forecaster

Riding Areas

Updated Mon, December 02nd, 2019

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.
Placer River	Closed	Closed.
Skookum Drainage	Closed	Closed.
Turnagain Pass	Closed	Closed.
Twentymile	Closed	Closed.
Seward District
Carter Lake	Closed	Closed.
Lost Lake Trail	Closed	Closed.
Primrose Trail	Closed	Closed.
Resurrection Pass Trail	Closed	Closed. Will be open for the 2019/20 season pending adequate snow cover.
Snug Harbor	Closed	Closed.
South Fork Snow River Corridor	Closed	Closed.
Summit Lake	Closed	Closed.