Surface Hoar
Learning Goal 7i. Describe the atmospheric conditions for surface hoar formation and how this might lead to an avalanche
Fig. 7i.1 Surface hoar crystals glistening in the
sun. (Credit: COMET/UCAR.)
Here are some definitions and reminders that will help you with this
section:
- Deposition occurs when a substance undergoes a phase change
directly from the gas to the solid phase, without the liquid stage in
between. For instance, the deposition of water is when it changes from
water vapour (gas) into ice (solid) without passing through the liquid
water phase. It literally deposits itself onto the snow surface.
- Dewpoint temperature is the air temperature at
which water vapour starts to
condense into liquid droplets, while being cooled. This concept was
introduced in Flying Module 1h.
- Frostpoint temperature is the dewpoint
temperature if the air is below 0°C. Instead of dew, frost forms.
What is surface hoar?
Surface hoar or hoarfrost or
just frost is essentially the frozen version of dew.
It is produced by deposition onto the snow surface when the
air temperature falls below the frostpoint temperature. The
outcome is the formation of ice crystals on the top of the snow surface.
Fig. 7i.2 - Surface hoar. (Credit: Howard.)
What is needed for surface hoar to form?
- Clear skies, usually at night, causing the
snow surface temperature to decrease greatly due to radiative cooling.
- Calm or near-calm winds,
less than 15 km/h. A small amount of wind is necessary to deliver new
water vapour supplies as the water vapour deposits onto the surface as
ice. This small amount of wind can be provided by subtle downslope
flows (Learning Goal 6b).
- A strong temperature inversion (Learning
Goal 6c)
just above the snow surface, usually a result of clear skies and calm
winds. This means that the air just above the snow surface is relatively
warm, around 10°C warmer or more, compared to the snow (even
though the air is often still quite cold).
- The size of the hoarfrost depends on how long the weather
conditions remain
this way, although it can form in just a few minutes. If it forms for a
prolonged period, it can reach several centimetres in size (Fig. 7i.3).
- Hoarfrost can keep forming into the daytime on north-facing
slopes that are in
the shade, because they continue to cool radiatively with little or no
heating from the sun. On these shady slopes, it may not melt during the
day. If there is a high pressure system, it can continue to grow night
after day after night.
- Surface hoar forms best on a flat, open surface. If there are
trees or rocks very close by this may
inhibit formation due to radiative warming from these "objects". This
warming prevents the snow surface from cooling down as much as it would
otherwise. For this reason, surface hoar coverage can vary greatly
between forested areas and treeless areas, such as clear cuts or slide
paths (paths that have been cleared by previous avalanches or
landslides).
Fig. 7i.3 Surface hoar that has formed over a long
period, perhaps all night and into the next morning. (Credit: West.)
What hazards does surface hoar present?
Surface hoar can lead to avalanches. As you can see from the
photographs (Figs. 7i.1-7i.4), surface hoar is very feathery and
delicate. When it's on the snow suface, it presents no danger. Once
it's buried by subsequent snowfall, however, the surface hoar acts as a
weak layer within the snowpack. With a layer of snow on top, the
hoarfrost layer is prone to collapsing easily, since there are very few
bonds between ice crystals and lots of empty air space,
compared with the rest of the snowpack. This can cause an avalanche.
If the surface hoar is uniform over a large area, as may happen in
alpine areas after a long period of high pressure, the weakness may be
widepread. With these conditions, larger
slab avalanches are more likely (Learning Goal 7j). This is where a large area of the
slope fails and slides downhill.
Further, this weak layer can sometimes remain buried for weeks. This
would be called a persistent weak layer .
The gradual accumulation of snow on top (which may be a metre or more
over a few weeks) may or may not be enough to trigger an avalanche.
However, if it gets just the right trigger, such as a heavy snowmobile,
the weak layer can fail, potentially leading to a large, destructive
avalanche.
Backcountry users, avalanche forecasters, and ski patrollers dig
snowpits to assess the different layers in the snowpack. This is one
way to determine whether a layer of buried surface hoar is present.
What destroys surface hoar?
- Sunlight or warm air causing sublimation
(phase change from ice directly to vapour).
- Strong winds, either by sublimation again, or mechanically, if
the wind is so strong it blows the light feathery crystals away.
- Melting/refreezing e.g. during the daytime.
- Rain or freezing rain.
After a long period of high pressure where there has been
significant surface hoar formation, backcountry users hope the first
storm that comes in starts off warm. In these cases, warm winds ahead
of the storm may largely eliminate the surface hoar (and its associated
danger). Also with a warm storm, the precipitation may start as rain,
which would also eliminate the surface hoar.
Fig. 7i.5 Surface hoar glistening in the sun.
(Credit: Howard.)
Key words: deposition, dewpoint, frostpoint,
surface hoar, hoarfrost, frost, slab avalanches, persistent weak layer
Figure Credits: Howard: Rosie Howard, West:
Greg West, Stull: Roland Stull