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skredfaren

Skredfaren is the term used to describe the risk of rapid mass movement in snow-covered terrain, most commonly snow avalanches (snøskred), but also including other forms of mass movement such as landslides. In Norway, skredfaren is a central part of winter safety, land-use planning, and backcountry decision-making, and is monitored by public authorities and emergency services.

Assessment and communication of skredfaren are typically done on a scale from 1 to 5, where higher

Causes and factors contributing to skredfaren include snowpack instability, weather conditions (heavy snowfall, rapid warming, rain-on-snow

Safety implications are addressed through public advisories and forecast updates. Travelers and outdoor enthusiasts are advised

See also: avalanche forecasting, skredvarsling, Varsom.

numbers
indicate
greater
danger.
Forecasts
and
danger
maps
are
updated
daily
during
the
snow
season
and
are
published
by
authorities
such
as
the
Norwegian
Water
Resources
and
Energy
Directorate
(NVE)
in
collaboration
with
the
Norwegian
Meteorological
Institute,
and
disseminated
through
services
like
Varsom.
events),
wind
loading,
temperature
fluctuations,
and
terrain
features
such
as
slope
angle
and
aspect.
Weak
layers
within
the
snowpack
can
trigger
avalanches,
especially
on
slopes
steeper
than
about
30
degrees.
While
snow
avalanches
are
the
primary
concern,
other
forms
of
mass
movement
can
also
influence
the
overall
hazard
in
a
given
area.
to
check
current
skredfaren
before
trips,
travel
with
companions,
carry
avalanche
safety
equipment
(beacon,
probe,
shovel),
and
adjust
routes
or
plans
according
to
the
forecast
and
observed
conditions.