If you're skiing off-piste this holiday weekend then you should be hoping for the same thing! As hot days and clear cold nights is what it will take to build a nice smooth melt-freeze layer. It is forecast to do just that.
Be careful of slopes above you. There's been a lot of new snow over the last few days in much of the Norther and Southern French Alps. Some big avalanches will be coming down as the slopes warm up - this will be especially true near the Italian border.
See below for a summary on what real spring skiing is (not slush) and how the melt-freeze layer can make for a great day out.
SPRING SKIING and the Melt-freeze Layer
Melt-freeze Cycles: Understand the ‘melt-freeze cycles’ and have fun with spring skiing!
Once the new snow
melts during the day and then freezes at night (1 melt-freeze cycle) a few
times in succession after a snowfall, the top snow layer begins to form a crust
that gets deeper and stronger after each melt allows free water to drip down
and re-freeze during the night. Any given ‘melt-freeze’ layer becomes stronger
with each cycle of melting and freezing due to the deeper penetration of each
melt during the day, which then adds more depth to the potential frozen layer
at night. If untouched, the top of this frozen layer is smooth and solid first
thing in the morning, then it becomes progressively softer as the warm sun and
increased temperatures melt it as the day goes by. This process starts on east
faces because they get the sun first thing in the morning, then south, then
west (north faces at 2500 metres don’t normally get a melt freeze layer on them
until late April due to lack of sun).
For good skiing!
The trick is,
after a couple of good melt-freeze cycles have created a solid layer on a
slope, you need to get on that slope when the snow surface is smooth and solid
with only 2 or 3 cm’s of soft melted snow on top (these are generally slopes
that have been in the direct sunlight only for an hour or so e.g. an East
facing slope at 9 or 10). Then you need to get off those slopes when the snow
surface begins to get too soft and mushy or you’ll start breaking through,
which is dangerous for your knees. AND the slope may be unstable due to all the
melting - then avalanches can be a problem.
In sum:
After a solid
melt-freeze layer has formed and there has been a good melt during the day, it
needs to freeze well the night before; the ideal is a cool clear night with
minimums of –2 degrees (or lower) at 2000 m. This will allow the melted parts
of the layer to freeze solid again from that altitude up. Then, in the morning,
you look to get on the east facing slopes first thing, 9 AM, because the sun
rises in the east and therefore those slopes get the sun first. Then you move
to south facing slopes, then west. Do this right and get some of the best
skiing of the season.
Aside from a night that is not cool enough, the only thing that gets in the way of great spring skiing is the nasty ruts in the snow that people leave behind because they either ski spring snow slopes (slopes that get lots of sun in spring: E,S and W) before the melt-freeze layer has formed or they ski the slopes too late when they are too soft and mushy.
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