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  1. #976
    Join Date
    May 2007
    Location
    Mt. Baker
    Posts
    1,754
    Quote Originally Posted by kamtron View Post

    I guess no matter what (whether or not we want to call it a PWL or just a possible sliding surface), when we get such large amounts of snow stacking up so fast, it's best to take a conservative approach as the snowpack adjusts to the added load. And luckily, burying such a crust layer deep enough (many meters down) should lead to a favorable situation for rounding over time due to reduced temp gradients.
    Dont get caught up in the terminology. PWL do not have to just be facets, depth / buried hoar, etc. An ice layer is in fact persistent and it can in fact be a weak layer, so thus it can be a PWL.

    Anytime you have a crust / ice layer in a snowpack near crust facets will form regardless of how that crust was buried. Water vapor is always moving up in the snowpack, crusts interfere with that and thus facets will start to form. Facets are also extremely strong in compression and can hold up a ton of weight before they fail. When that actually happens is anyones guess. Ideally we get enough rain to either force that failure along prematurely, or enough water to percolate down and saturate those facets and and then refreeze. Of note some of the biggest sides I've seen at baker involved a crust, where the snow came in correctly on top of it and started off being well bonded. Then it eventually failed months latter after a ton of snow fall. It is also worth noting, that typically in January we have a very stout crust form followed by a cold dry spell (January is usually high and dry here) then lots of snow usually buries it in Feb. So every major slide that has occurred (15+ feet deep) around the ski area has been with in the week before / after March 15th.

    The current situation was made worse, sooner by the crust being buried by a layer that didn't stick to it from the beginning, creating a sliding surface that would reload and slide multiple times.

    At the end of the day, one of the most dangerous things you can do is to "over think" snow science as anytime you think you can "out smart" a problem you will get spanked. The most important thing for me, when evaluating hazard is constantly asking what's going on thats out of the ordinary? Did we get a big loading event? Was there unusually strong winds? An unusual wind DIRECTION? A unusual dry period? unusual temps? unusual natural slide activity? The list goes on, but anytime anything unusual is on my radar, then I use a lot of extra caution as thats when "unusual" things such a slides, etc will tend to happen.

    An unusual wind direction is a big one for me. Anytime a North East system comes in, which usually results in high-pressure we get very cold and very strong winds out. of the NW. That always scrapes snow off of the best ski terrain at Baker and then loads a lot of the terrain that is usually safe even on high avalanche danger days.

  2. #977
    Join Date
    Nov 2006
    Location
    NCW
    Posts
    4,605
    10" of new under light to pissing rain at the windy hill this morning. Steep natural snow was velvety but in classic Mission fashion they sent the cats out in the evening on the only open chair worth riding, so it was 500 vert to 3" of garbage velcro mush on the "groomed" slopes. One and done for me and the missus, not worth a knee injury.

    Hoping for percolation and consolidation of the pack.

  3. #978
    Join Date
    Jul 2008
    Posts
    3,673
    Quote Originally Posted by Gunder View Post
    Dont get caught up in the terminology. PWL do not have to just be facets, depth / buried hoar, etc. An ice layer is in fact persistent and it can in fact be a weak layer, so thus it can be a PWL.

    Anytime you have a crust / ice layer in a snowpack near crust facets will form regardless of how that crust was buried. Water vapor is always moving up in the snowpack, crusts interfere with that and thus facets will start to form. Facets are also extremely strong in compression and can hold up a ton of weight before they fail. When that actually happens is anyones guess. Ideally we get enough rain to either force that failure along prematurely, or enough water to percolate down and saturate those facets and and then refreeze. Of note some of the biggest sides I've seen at baker involved a crust, where the snow came in correctly on top of it and started off being well bonded. Then it eventually failed months latter after a ton of snow fall. It is also worth noting, that typically in January we have a very stout crust form followed by a cold dry spell (January is usually high and dry here) then lots of snow usually buries it in Feb. So every major slide that has occurred (15+ feet deep) around the ski area has been with in the week before / after March 15th.

    The current situation was made worse, sooner by the crust being buried by a layer that didn't stick to it from the beginning, creating a sliding surface that would reload and slide multiple times.

    At the end of the day, one of the most dangerous things you can do is to "over think" snow science as anytime you think you can "out smart" a problem you will get spanked. The most important thing for me, when evaluating hazard is constantly asking what's going on thats out of the ordinary? Did we get a big loading event? Was there unusually strong winds? An unusual wind DIRECTION? A unusual dry period? unusual temps? unusual natural slide activity? The list goes on, but anytime anything unusual is on my radar, then I use a lot of extra caution as thats when "unusual" things such a slides, etc will tend to happen.

    An unusual wind direction is a big one for me. Anytime a North East system comes in, which usually results in high-pressure we get very cold and very strong winds out. of the NW. That always scrapes snow off of the best ski terrain at Baker and then loads a lot of the terrain that is usually safe even on high avalanche danger days.

    I love your takes, and if I’m reading correctly your general gestalt, I totally agree. I worked in the snow for many years prior to moving in a different direction and had many excellent teachers, but one who stood out was the one who always taught to not get bogged down in the minutia of snow science. Look at the big picture, simple stuff and you can stay alive a very long time. When I was back in my formal AIARE days I always thought that there was too much diving into the snow science, which while great! I feel like is often hard for layman to use effectively and simply. Maybe there is a new approach being used.
    Do I detect a lot of anger flowing around this place? Kind of like a pubescent volatility, some angst, a lot of I'm-sixteen-and-angry-at-my-father syndrome?

    fuck that noise.

    gmen.

  4. #979
    Join Date
    Oct 2008
    Location
    Wenatchee
    Posts
    14,731
    Quote Originally Posted by jackattack View Post
    10" of new under light to pissing rain at the windy hill this morning. Steep natural snow was velvety but in classic Mission fashion they sent the cats out in the evening on the only open chair worth riding, so it was 500 vert to 3" of garbage velcro mush on the "groomed" slopes. One and done for me and the missus, not worth a knee injury.

    Hoping for percolation and consolidation of the pack.
    I can’t believe you put your boots on


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  5. #980
    Join Date
    Nov 2006
    Location
    NCW
    Posts
    4,605
    Quote Originally Posted by MagnificentUnicorn View Post
    I can’t believe you put your boots on
    gambled and cut our losses.

  6. #981
    Join Date
    Jan 2008
    Posts
    1,248
    Quote Originally Posted by jackattack View Post
    gambled and cut our losses.
    I stood there for awhile. Went home injury free.

  7. #982
    Join Date
    Nov 2006
    Location
    Wenatchee, WA
    Posts
    782
    I did 3 laps in the trees off 3 (which were pretty decent) but yeah, as soon as you hit the groomers it became glue. Easy call to pull the plug on the day
    "No snowflake in an avalanche ever feels responsible" -Stanislaw Jerzy Lec

  8. #983
    Join Date
    Oct 2003
    Location
    Seattle
    Posts
    5,365
    Quote Originally Posted by Norseman View Post
    Good post about this from a southern neighbor (post 842 in the Oregon thread):
    This video I just saw posted on near crust faceting seems relevant to the discussion:


  9. #984
    Join Date
    Mar 2012
    Location
    West Side WA
    Posts
    483
    Thanks for the video! About 10 min in he talks about possible outcomes in a maritime snowpack.

    Here's some stoke for you all. First picture from Dec 23, one day after a solid rain event, a good day for facet atop crust surfing.
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  10. #985
    Join Date
    Oct 2003
    Location
    Seattle
    Posts
    5,365
    ...crickets..... well it's at least sunny?

  11. #986
    Join Date
    Sep 2006
    Location
    Seattle
    Posts
    880
    Click image for larger version. 

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    Surprised there isn't more from Saturday coming in.

  12. #987
    Join Date
    May 2002
    Posts
    690
    no shit! keep em coming.

  13. #988
    Skis's Avatar
    Skis is offline It's one louder, isn't it
    Join Date
    Apr 2007
    Posts
    378

    Stevens vs crystal for a week in late February?

    Any idea how the crowds have been with COVID rules at each place? Mostly thinking midweek, but probably end up doing a couple weekend days too. Other thoughts?

  14. #989
    Join Date
    Aug 2014
    Location
    Imaginationland
    Posts
    4,798
    Weekend days? You must like lines.

  15. #990
    Join Date
    Feb 2012
    Posts
    10,958
    Quote Originally Posted by Skis View Post
    Any idea how the crowds have been with COVID rules at each place? Mostly thinking midweek, but probably end up doing a couple weekend days too. Other thoughts?
    Totally!


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  16. #991
    Join Date
    Oct 2003
    Location
    Seattle
    Posts
    27,359
    Quote Originally Posted by Skis View Post
    Any idea how the crowds have been with COVID rules at each place? Mostly thinking midweek, but probably end up doing a couple weekend days too. Other thoughts?
    If you don't like lines head up for night skiing. Obviously that limits the terrain options, but you can lap to your heart's content.

  17. #992
    Join Date
    Oct 2010
    Location
    Seattle
    Posts
    271
    My Crystal experience so far: lines are longer on weekends but not by much. In a normal year, midweek would have zero lines but now they are about 75% of what the weekend lines are so it isn't a huge benefit going midweek. Lines are significantly smaller after around 2PM or so. Also, depends a lot if all lifts are running or not, windhold = huge lines.

    Every midweek day I have skied this year the parking lots were filled into F lot.
    You Will Respect My Authoritah!

  18. #993
    Join Date
    Oct 2003
    Location
    Seattle
    Posts
    5,365
    Quote Originally Posted by timeo View Post
    My Crystal experience so far: lines are longer on weekends but not by much. In a normal year, midweek would have zero lines but now they are about 75% of what the weekend lines are so it isn't a huge benefit going midweek. Lines are significantly smaller after around 2PM or so. Also, depends a lot if all lifts are running or not, windhold = huge lines.

    Every midweek day I have skied this year the parking lots were filled into F lot.
    I concur, although maybe on one day I skied the G lot didn’t fill. It’s been busy for sure.

  19. #994
    Join Date
    Jan 2017
    Location
    Seattle, WA
    Posts
    2,206
    I would say COVID-19 restrictions are much tighter at Crystal than Stevens. Crystal has lifties running the lines but at Stevens it was a lot easier to casually pair up. Also, mask enforcement was much stricter at Crystal where they yell at you constantly whereas my experience at Stevens (only one time) is that when you get to the ropes for the lines you should pull your mask up but its more casual and less yelling.

    Don't mind either way, but lines seemed to move faster at Stevens.

  20. #995
    Join Date
    Oct 2010
    Location
    Seattle
    Posts
    271
    I will also add that the singles line moves twice as fast as the other lines on Rex based on how they have been loading, they have just been taking a group from each line on Rex which means they take two singles each pass. This is the only chair that works this way because it has one single line vs. two single lines at the other chairs.
    You Will Respect My Authoritah!

  21. #996
    Join Date
    Jan 2008
    Location
    livin the dream
    Posts
    5,778
    Quote Originally Posted by timeo View Post
    I will also add that the singles line moves twice as fast as the other lines on Rex based on how they have been loading, they have just been taking a group from each line on Rex which means they take two singles each pass. This is the only chair that works this way because it has one single line vs. two single lines at the other chairs.
    As a single you get fucked during the morning rush on Chex. They don’t load a singles chair like they do on Rex.... it will take 2-3 times longer to load than a group of two...


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  22. #997
    Join Date
    Oct 2004
    Location
    Seattle
    Posts
    3,763
    Posted this in the Alpental thread, but Snoqualmie reposted Thing #2 getting huge at Alpental.

    https://www.instagram.com/p/CKEek2sh...d=gssic473fsa6

  23. #998
    Join Date
    Feb 2008
    Location
    Alpental
    Posts
    4,172
    Mission Ridge has it going on after the lifts close Click image for larger version. 

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    “I have a responsibility to not be intimidated and bullied by low life losers who abuse what little power is granted to them as ski patrollers.”

  24. #999
    Join Date
    Feb 2012
    Posts
    10,958
    Quote Originally Posted by snoqpass View Post
    Mission Ridge has it going on after the lifts close Click image for larger version. 

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    And powdered snow.


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  25. #1000
    Join Date
    Jan 2008
    Posts
    1,248
    It got real busy there for a while.

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