Happy Holidays from NWAC!
We hope you have gotten out a few times this winter to enjoy our early November snowfall and recent sunny (if COLD) weather. It's been quite a start to winter for sure, and hopefully we'll see some new snow for the upcoming holidays.
That said, take a look at the blurb below about the snowpack. The still relatively shallow snowpack and cold temps of early December have resulted in quite a bit of faceting and some real weak layers. Be careful out there as the new snow loads those layers. Things could get dicey and stay that way for a while.
On another topic, we have gotten a lot of positive feedback about the new NWAC website, and some really constructive suggestions as well. We'll be launching into phase two of the upgrade soon, so please keep those suggestions coming as we work to make the site the best avalanche forecasting website in the US.
The new site has also generated quite a few new memberships and we thank those who have joined the cause in the past couple of months. You all rock! To those who have not yet joined, please consider becoming a member. Your year-end contribution is tax deductible and will help us continue to support NWAC and grow our avalanche education program.
Here's to a snow filled holiday season and a cold, white New Year!
The Friends of NWAC
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Beware the Sketchy Snowpack
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By Mark Moore, NWAC Director
While the early season snowfall was welcomed by all of us
who like to play in it, the recent cold snap has wrecked some havoc with it.
Many areas of the Cascades and Olympics have experienced and are experiencing
significant faceting...both above a slightly decomposing mid-upper pack crust
(near surface facets) and below the crust all the way to the ground. This is just beginning to create intermediate
faceting, not depth hoar yet, for most
Cascade west side areas, but the generally shallower Cascade east slope snowpack
is dominated by facets and quite sugary with some true depth hoar (well
developed columnar shapes) likely near the ground.
In general faceting occurs most quickly when air temps are close to freezing since
the vapor pressure is highest there and thus there is more vapor to be deposited
or transferred as new facets. The change in vapor pressure per degree temperature
change is highest at these temperatures, hence facets or depth hoar develop near
the ground where it's normally close to freezing. This gradient in the snowpack
is by no means static or average, with maximum temperature gradients often
above higher density layers like crusts (the crust conducts the heat well, but
the lower density snow above the crust does not = high gradient). Below crusts, the vapor is deposited because
it accumulates (it has nowhere to go since the crust provides a cap). The end result is that the near-surface facets
and surface hoar will provide plenty of weak layers that may linger for some
time.
With the more normal Cascade loading that we have seen
recently, and are likely to see more of, we can expect the development of slabs
(and the resulting sympathetic fractures, remote triggering, cracking and
whumpfing). The combination of slabs and weak layers is,
as many of you know, what results in dangerous avalanches. In areas where a shallower and more faceted
snowpack exists, there could be climax slides to ground.
The take home message...be careful and aware that weak layers
have developed and could linger for some time.
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Check us out on Facebook
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The Friends of NWAC have joined the social media revolution! We hope you will become a fan on Facebook where we will try to keep regular updates coming about everything avalanche related in the Northwest.
While the site is not intended as a substitute for checking the forecast at nwac.us, we will be posting avalanche warnings when they occur in addition to other relevant information such as upcoming classes and events, as well as announcements from our sponsors and links to pertinent articles and other educational info.
Sign up now and stay in the loop!
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Upcoming Classes and Events
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The Friends of NWAC
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