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Weak layers in the snow pack

 Poster: A snowHead
Poster: A snowHead
Im sure i watched a film of Ross Hewitt and company skiing last week and at the beginning of the film it showed one of the gang scoop up a hand full of Hoar crystals?? Hopefully the correct name for them and I was wondering if these conditions we are having now are the perfect ones for producing the problematic weak layers for later in the season, hopefully someone will know how long it takes for them to develop.
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Obviously A snowHead isn't a real person
Pretty much as you watch. So I don't actually know as I have not sat around watching it, but I think it forms quickly, within an hour or two. Typically you see it (in BC) in the late afternoon as it's cooling down. I guess the air has a fair bit of moisture from sun during the day and as the sun goes down the temperature drops quickly, bringing the amount of moisture the air will hold down. As that condenses out (not sure if that's the best term - the reverse of "sublimates" anyone?) it forms crystals which are typically large. I'm not sure precisely what governs the typical/ maximum size, but it's huge compared with the structure of the snow itself. Hence the mismatch when you try to get it to form up.
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@philwig, I know in previous seasons recently early season snow then lack of it for the next couple of weeks up to a month has seen significant problems with this I just wondered if its heading that way.
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I haven't seen any surface hoar this season but I've seen a lot of facetted snow, I posted a video on the snow conditions thread where the whole snowpack at the top of a couloir comprised these type of crystals. Round here you normally get surface hoar at lower elevations (frequent between 1000-1800m) where it is sheltered, there isn't any snow at lower elevations at the moment in France where I'm based so no surface hoar.

By the time it snows next the whole snowpack on north sectors could be facetted crystals. So expect a lot of 2/4 days where the avalanche risk rises from 2 to 4 at around 2200m where the current snow can be found. It could surprise a few people but not snowheads Happy


Last edited by You need to Login to know who's really who. on Tue 6-12-16 20:58; edited 1 time in total
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I@davidof, is this only relevant to north facing slopes or can this be a problem on all aspects?.
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Right that makes sense as the were just setting of from somewhere low down and thats when a hand full where scooped up like little glass shards....unless ive dreamt this Puzzled Very Happy
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Then you can post your own questions or snow reports...
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After all it is free Go on u know u want to!
meandrew wrote:
Right that makes sense as the were just setting of from somewhere low down and thats when a hand full where scooped up like little glass shards....unless ive dreamt this Puzzled Very Happy


It often forms around the dew point - it is extremely unpredictable though. You can ski through trees, into a clearing and bam, the forest clearing goes because surface hoar formed there just before the latest snowfall. As we know, avalanches and trees are not a good mix.
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That looks pretty terrifying to me and has given me a much needed kick up the back bottom to educate myself better this season.
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Interesting info I really need a course to go on to get so knowledge into me. Thanks@davidof,
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If you look at the Tremper book (Staying Alive in Avalanche Terrain) he explains things very well. For slope aspect see P78. For Switzerland he gives N -> NE -> E as the critical aspects.

It is worth reading his book but there is really too much information to retain everything. Guide Olivier Mansiot says that carefully reading the avalanche bulletin for your sector and keeping off slopes they warn against is the most important factor.
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Thanks I will have a look for that and local knowledge is always a given and taking any warnings given seriously I am always cautious and probably sometimes over cautious and thats another good reason to educate myself more as im probably missing out sometimes.
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Just noticed this after posting similar photos in the general thread.

Deep in a shaded valley in Tirol that gets no sun at this time of year:



I assume this is the case on shaded N slopes at altitude too, but haven't been up to look in a few weeks.
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 You know it makes sense.
You know it makes sense.
@clarky999, thats the stuff Ive seen recently im glad Im not going mad Very Happy
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 Otherwise you'll just go on seeing the one name:
Otherwise you'll just go on seeing the one name:
clarky999 wrote:


I assume this is the case on shaded N slopes at altitude too, but haven't been up to look in a few weeks.


That looks like surface hoar, I assume it was the crystals sitting on top of the snow? It is depth hoar (gobelet) and near surface faceted snow on N slopes at altitude at the moment formed by a temperature gradient in the snowpack. Surface hoar tends to form at low to mid altitudes - below temperature inversion (which is probably why Clarky found it) or near the dew point.
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