Sluff Management:
by Jim Conway and Mark Newcomb
as presented at the International Snow
Science Workshop 1998
ABSTRACT: Since the first World Extreme Skiing Championships
in Valdez in 1991, the Chugach Range around the Thompson Pass
area has drawn thousands of skiers seeking steep powder and
adventure skiing. The spring season often provides “windows”
of stability which allows skiers and snowboarders to push into
steep, technical, and exposed terrain. The steepest slopes now
descended by heli ski operations in the area range from 40 to
60 degrees. While these “windows” of stability may
have low hazard in terms of slab potential, sluffs and small
point release avalanches remain a hazard. Over the last five
years the staff at Valdez Heli Ski Guides have observed the
interaction of skiers/boarders with sluffs in various terrain
scenarios. The term “Sluff Management” was developed
to describe the various techniques of avoiding and managing
this hazard.
The presentation will describe the types of terrain and snowpack
where sluffs become a significant hazard that needs to be
managed. It will also review the recent evolution of powder
specific skis and snowboards and how this relates to managing
sluff hazards. Real life examples will be used to represent
various scenarios depicting a number of Sluff Management techniques.
Many of the techniques to be reviewed have proven significant
in reducing the risk of an incident negotiating the steep
terrain in the Central Chugach area.
1. Introduction:
Due to advances in equipment, hype from the media, and changes
in attitude, the demand for the steep skiing experience has
increased over the last ten years. While not a mainstream
activity, steep skiing has certainly risen above the “fringe
sport” category within the skiing community. Concurrent
with this development was the rediscovery of Alaska’s
Chugach range as a premier steep skiing center. The first
World “Extreme” Skiing Championships in 1991 exposed
many avid backcountry and hard core skiers to the areas potential.
Within three years the first commercial guiding operation
was established. Now, there are four commercial heli ski operators
in the Valdez area, three of which specialize in the steep
skiing experience.
At Valdez Heli Ski Guides, this evolution has resulted in
an economically viable guide operation that caters to clients
who desire an adventure experience. The ability of the client
varies from the well conditioned expert to world class skiers
and boarders. Even the least experienced clients possess the
athletic ability and competence to negotiate some very challenging
terrain, but they may not have the necessary mountain or snow
skills required. A great deal effort, beginning with a thorough
safety briefing, is devoted to education on avalanche hazard,
glacial travel, and respect for the mountain environment.
For the clients, guide direction and coaching is critical
for reducing the risks. Terrain is selected for each client
based on their skills, experience, desire, and ability to
follow the guides recommendations. Clients start off on easily
manageable slopes and gradually progress into more challenging
terrain (“Terrain Progression”).
Once stability has been established, and suitable terrain
has been selected, the hazard most commonly encountered on
steep slopes is sluffs. The guide staff, through the use of
basic backcountry protocols (i.e. skiing one at a time), observation,
and some hard learned lessons, has developed a method labeled
“Sluff Management”. The goal is to reduce one
of the many risks involved in traveling in a winter alpine
environment.
2. Defining a Sluff:
For the purpose of this discussion, a “sluff”
will be considered a small loose snow avalanche. Often the
sluff will be the result of a series of point releases in
the starting zone. The depth of the layer, for manageable
sluffs to which this paper refers, can range from 3 to 15
cm. Skiable slopes likely to sluff range from 40 to 60 degrees.
Observed speeds, estimated in the field, range from 5 to 25
meters/second. The density of the snow involved is typically
5 to 15%. The snow is new snow, decomposing precipitation
particles, or near surface faceted crystals. The highest potential
involves near surface faceted snow. Sluffs have been observed
up to two weeks after the last storm event on the steeper
slopes. The father out from a storm event, the more likely
the sluff layer is composed of facets. Most of these events
do not result in significant deposition in the runout (0.0
to 0.4 meters).
3. The Need for Management:
Although burial is a possibility, basic terrain selection
usually removes this risk (i.e.: avoiding terrain traps).
The hazard comes from the sluff causing a high speed fall
down steep, and in some cases, exposed terrain. Injury due
to trauma may result. This may be caused by impact with other
objects or simply over stressing the body in a violent tumble.
The slopes descended vary from 500’ to 2000’,
and range from 40 to 60 degrees. Exposure may consist of cliffs,
seracs, bergschrunds, or crevasses. Bergschrunds lying below
many steep faces are the most common hazard, especially when
the gap is wide, or the downhill edge of the gap is higher
than the uphill (“Innies”). The ultimate goal
of sluff management is to avoid interaction with a sluff event.
4. Sluff Management Techniques:
Avoidance by Speed
- This can be described simply in two ways. Go slow enough
to stay above the sluff in the starting zone. Or, go fast
enough to beat it through the runout zone. Obviously the technique
used depends upon the skiers ability and snow quality.
Avoidance by Terrain
- Proper terrain selection can eliminate exposure to a sluff
event. The simplest technique is to ski off falline to one
side in the starting zone. A variation of this is to ski down
an appropriate number of turns (depends on the dynamics of
the sluff) then traverse off to one side, out of the sluff
path, and begin turning again. As long as there is enough
room laterally, whole slopes can be descended using this technique.
Another method is to ski slopes with a double falline so the
sluff is constantly moving downhill and away. Finally, spines
(steep snow ridges) are another good terrain feature, as the
snow falls to either side and away from the skier. The spine
must be big enough that the skis are not near the right or
left edge of the spine where it meets the sluff path. A skier
must also be alert if a spine ends at a point where the sluff
path on either side converges. In all cases, care must be
taken to avoid terrain features which enhance the sluff, such
as gully bottoms and narrows.
Avoidance by Combined Techniques
- On complex terrain, combining the above techniques is the
best way to mitigate the sluff hazard. Their are countless
variations of speed and terrain use that can be successfully
executed. The most basic technique is to ski down to an Island
of Safety, stop, wait for the sluff to pass, then continue.
A necessary skill for effective use of the combined technique,
is the ability to look up hill while skiing and track the
progress of the sluff (also known as the “Chugach Look”).
A common scenario is to aggressively descend in front of a
sluff, then as the skier observes it catching up, he pulls
off onto a slope with a new falline and drainage. The original
sluff continues down the first drainage while the skier has
transferred to the new drainage. A skier might just as easily
ski up onto a spine or a side slope with a double falline,
watching for the sluff to pass before reentering the original
falline. A number of these maneuvers may have to be incorporated
into one run. Obviously, this is a more advanced technique
requiring careful study of the terrain along with mental and
athletic skill.
Ski Cutting
- Ski cutting is probably the most traditional method of controlling
sluff activity. In many cases it will serve to eliminate the
chance of sluffing during a run. On the other hand, enough
loose snow may remain to create a substantial hazard, especially
on the steepest slopes. But the experienced steep skier may
be reluctant to cut slopes for aesthetic reasons. This might
be for the pure powder experience or a film shoot. Where the
skier is confident in his ability to negotiate the terrain
and sluff paths, he may prefer to deal with the sluff during
the run, rather than control it ahead of time. The guide,
through communication with the client, determines what is
advisable in each situation.
6. The Sluff Management Plan:
From the straight forward run descended by a skilled but
unpracticed client, to the complex lines of a world class
skier or boarder, a sluff management plan is the key to reducing
risk. A sluff management plan is the result of careful study
of the terrain , snow conditions, skiers ability, and contingencies.
It puts together all of the techniques described above into
a comprehensive plan. It is key that the client is thoroughly
briefed on his line and options before he begins the run.
It can be as simple as pointing out a recommended line; or
as complicated as developing a plan that incorporates all
of the strategies above. The guide will point out the potential
sluff hazard to the client and will develop and/or approve
a plan. A guide must carefully consider the clients line and
be confident that he can execute it. If there is any doubt,
a more conservative line should be selected.
In situations where accomplished athletes drop big complicated
lines, time must be taken to thoroughly study the terrain
and snow. The group may land adjacent to the slope and study
it, or make use of Polaroid snapshots. Most guides use this
opportunity to educate clients about hazards and strategy.
For each big descent it is prudent that the guide works with
the pilot and other skiers to come up with contingency plans
in case of an incident. It is important to note here the standard
practice of pointing out the hazards and preferred line to
an average client, versus the extensive preparation involved
in setting up a major descent by a world class athlete. The
more complex the descent, the more dynamic the plan needs
to be with options based on forecasted contingencies.
6. Conclusions
The techniques for sluff management have become more complicated
due to two relatively recent events. One is the popularity
of snowboarding and especially freeriding. And the other is
development of wide high performance skis designed specifically
for fast high performance powder descents. Snowboarders took
the lead on establishing how fast steep terrain can be descended
in powder conditions. But in the past two years high performance
fat skis have allowed skiers to adopt the same aggressive
‘out in front’ sluff management tactics. Controlled
ski descents with speeds from 40 to 60 miles per hour have
been witnessed. In the past, the primary backcountry user
was most likely on narrow waisted skis. The limitations imposed
by this equipment usually forced the skier to descend slowly
and deal with sluffs high in the starting zone, staying high
enough where the forces are less powerful. Now with the higher
speeds allowed by snowboards and fat skis, the rider has the
potential to be affected by the sluff much lower in the track
where the forces are much greater. The new technology, even
in the hands of the average backcountry skier or heli ski
client, has exposed even more users to this hazard.
The staff at Valdez Heli Ski Guides has had a strong measure
of success using the techniques described above. Fortunately,
to date there have been no serious incidents as the result
of a skier or guide being involved with a sluff. The practice
of the techniques described in this paper clearly reduce the
risk of an incident.
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