Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 3rd, 2020–Jan 4th, 2020

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely.

Regions

Olympics.

Fresh wind slabs will build on lee slopes as snow levels drop tonight and winds continue to move snow through Saturday. Avoid steep wind loaded slopes over 35 degrees by sticking to lower angled or wind-scoured terrain. Give cornices a wide berth as you travel along ridgelines and avoid traveling on slopes directly below them. 

Discussion

A big warm-up on Friday brought plenty of wind (gusts into the 60s!) with rain falling uphill by the afternoon (according to Park Rangers) to Hurricane Ridge. Snow that was still available for transport in the morning quickly became moist with the warm-up. Observations were limited due to winds on the Ridge Friday. The roller coaster of snow levels in this active pattern will continue through the weekend, with snow levels plummeting overnight and a fresh round of snow and wind expected. Below 4500' (below treeline) low snow depths are still limiting the avalanche potential. By the end of next week and with additional cool storms, we may be able to change that story at lower elevations. Expect challenging travel conditions on steeper terrain that has been wind scoured down to the most recent rain crust.  

Forecast Schedule

For the 2019-20 winter season, avalanche danger ratings will be issued for the Olympics every Friday through Sunday and during mid-week holidays. During the week, No Rating will be issued but forecasts will include expected conditions and relevant travel advice.  If you are out in the Olympics, share your backcountry observations with us and the greater community.

Snowpack Discussion

January 02, 2020 (The regional synopsis is updated every Thursday @ 6 pm)

Happy New Year! 

The pacific northwest rung in the new year with a winter storm cycle that brought changing conditions to our region. This storm exhibited three characteristics: warm, wet, and windy. Let’s take a look at the end of 2019, the beginning of 2020, and where we can go from here. 

Wrapping up 2019

The last few days of December were generally quiet and cold. The snowpack seemed to enjoy this break in the weather. Lingering unstable snow from the pre-Christmas storms gained strength, persistent weak layers appeared to stabilize, and avalanche hazard decreased in all forecast zones. All in all 2019 ended quiet and uneventful… until the New Year’s Eve weather party showed up …  

Quiet weather led to lower avalanche danger during the last week of 2019. Hogsback, White Pass, WA. Photo: Andy Harrington

Blowing into 2020

A warm, wet, and windy weather system blew into the northwest for New Year’s Eve and New Year’s Day. This brought rapidly changing conditions and increasing avalanche hazard to all areas. 

  • Warm: Unfortunately this system brought with it warm air. Freezing levels measured near the coast reached 9000’ on the afternoon of the 31st. Many weather stations recorded above freezing temperatures during the onset of precipitation. 

  • Wet: While this system wasn’t as wet as the atmospheric river prior to Christmas, it still produced impressive water numbers in many areas. The bulk of the precipitation seemed to be focused on the Passes and Volcanoes, and water spilled over the crest to places like Washington Pass and Leavenworth. Sadly, when combined with the warm temperatures, this translated to rain well into the near treeline band (or higher) for most areas. The main exception appeared to be in the northeastern cascades, where locations like Washington Pass remained all snow. 

 

HurRidge

MtBaker

WaPass

Stevens

Leavenworth

SnoqPass

MtRainier

MtHood

Precipitation (in)

1.84

3.39

1.42

4.56

1.06

6.19

5.39

5.41

Snow (in)

-

15

-

12

0

3

10

8

Table 1: Precipitation and storm totals from selected weather stations during the New Year’s Eve Storm. “-” 24hr storm snow not measured. 

  • Windy: While the warm and wet were impressive, it’s the winds that may set this storm apart. Most weather stations recorded very strong and extreme winds during the storm. Alpental exceeded 100mph just after midnight to ring in the new year. Any dry snow at high elevations was redistributed by the wind and snow surfaces were transformed. 

Table 2: Wind speeds from New Year’s Eve from selected wind sites. Note the sustained period of winds between 40-60mph.

Eventually, temperatures cooled, the rain turned back to snow, and winds calmed. Many locations picked up additional snow as the storm wound down, but 2020 was already off and rolling with its first major storm.

New Year’s Resolutions

The active weather pattern that started the new year appears to continue. The snowpack and avalanche conditions will continue to change. So, what can your New Year Avalanche Resolutions be? 

  1. Read the forecast. This is a great way to monitor conditions even if you aren’t heading into the mountains. 

  2. Get out in the snow! Enjoy the wonderful mountains in your backyard. 

  3. Submit an observation. Tell the avalanche center what you saw while out in the snow by submitting an observation and sending in a photo. 

Thanks for all of your support in 2019 and here’s to 2020!

-Dallas

 

Problems

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.