By Keith and Heather Nicol
When ski touring
in the spring we need to be aware of snow safety if we travel in avalanche
terrain. If you are not sure if your planned
route is traveling in areas where avalanches
might occur you can check out the on line maps which show potential avalanche
start zones in Western Newfoundland. This map (
https://cb-grf-grfmap.cna.nl.ca/avalanche/V3/snowStyled.htm)
highlights areas that are between 30-45 degrees which are the typical slopes needed
to get avalanches moving. Simply click on the start zone symbol and if you want
to see where avalanches have occurred in the past you can click on the
avalanche symbol. You can zoom in and out on the map and you can also move
around to different areas in Western Newfoundland. As you can see there is lots
of areas where avalanches can start but there is also great low angle ski
touring that can be done in this area if you want to avoid avalanche terrain
altogether.
However, many backcountry
skiers and snowboarders want to ski steep areas in the Tablelands or Blow Me
Down Mountains and if you do you need to think about how to manage the various snow
safety hazards. In a typical Newfoundland spring there are 4 different types of hazard ranging
from cornice fall to loose wet snow avalanches as well as wet slab and wind
slab avalanches to consider. Cornices may fail at any time but in the spring the
risk goes up as the temperature rises above 0 C. Cornices not only are
dangerous in themselves but they might also trigger avalanches on the slopes
below as shown in the photo below from the Tablelands. So give cornices a wide
berth when skiing above and below them especially on warm days.
|
A large chunk of cornice that also triggered an avalanche (note debris up slope) |
Wet loose snow
avalanches are common in the spring in Western Newfoundland and the adjacent
photo shows several in Blow Me Down Bowl. These avalanches are generally not
too hazardous on an open slope but they do pack more punch than you might
think. They can often knock a skier or rider down and if there are rocks or
trees downslope they can possibly be injured. To manage this risk avoid start
zones when the snow is wet from the sun, warm temperatures, rain or does not
freeze overnight.
|
Large loose snow avalanches in Blow Me Down Bowl |
Wet slab avalanches
are more of a hazard than loose snow avalanches since they involve more snow
and will likely travel faster. They occur when water percolates into the snow
layers and triggers an avalanche. The photo below shows one that occurred in
the Tablelands Bowl. Although this slide was only 30 cm deep in most places it
did pile up to 1.5 meters in others and was an estimated 80-100 meters long. To
manage this risk avoid start zones when the snow is wet from sun and warm temperatures,
rain or does not freeze overnight.
|
Wet slab avalanche in Tablelands Bowl |
|
Wind slab avalanche |
Wind slabs tend
to occur where fresh snow has been deposited on lee slopes. Since we likely
will not get much new snow through the rest of this spring this hazard is not
that likely but if we do get a spring snow storm then be aware of where the
wind may have piled this snow up. Also since it likely will fall on an icy
crust this creates a good layer for this snow to slide on.
Since we get most of wind from the west this
hazard can be managed by avoiding steep east slopes where wind slabs are most
likely to have been created.