Density of Newly-Fallen Snow
Learning Goal 7b: Define snow density and describe what
conditions will lead to high vs. low density newly-fallen snow, and why
this matters to skiers.
What is snow density?
Snow density can be defined as the amount
or mass of ice and liquid water per volume.
You shouldn't worry too much about the liquid water part because there
is usually a LOT more ice than liquid water in the snowpack. However,
in the spring, liquid water content can be more significant. Snow
density measurements are usually not divided into ice and liquid water
components though, and it is the total (= frozen water +
liquid water) density that we are concerned with here anyway.
Fig. 7b.1 gives you a reminder of the range of snow densities you
will
find in a snowpack, although note that the characteristics here are not
constrained to newly-fallen snow. Newly-fallen snow is generally in the
30-300 kg/m3 range.
Table
7b.1 - Typical snow densities ranging from freshly fallen snow (lowest)
to solid ice (highest). (Credit: Stull)
Fig. 7b.1 - This
newly-compacted snow on this recreational race course is probably
around 350 kg/m3. Telluride, Colorado, USA.
(Credit: West)
The effect of conditions on newly-fallen snow
-
Temperature
Generally, the warmer the temperature, the higher
the density of newly-fallen snow. For
temperatures close to freezing, you can expect higher density snow,
partially because it has higher water content too (water is more dense
than ice,
which is why ice cubes float in water). To think of it the
other way, the lower the temperature, the lower the
density of newly-fallen snow. This relationship holds down to about
-15°C. At temperatures colder than that, density doesn't change much.
-
Wind
Similarly, with faster wind speeds, one can generally
expect higher-density newly-fallen snow. With slower
winds speeds, one can generally expect lower-density
newly-fallen snow.
The relationship between wind speed and snow density is weaker than
that between temperature and snow density.
For higher wind speeds around 15 m/s and above,
you're likely to encounter high-density snow. For low wind speeds, you
might get low density snow, but it's also possible to get high
densities (e.g., if temperatures are warm).
In summary, higher density newly-fallen snow comes with warmer
temperatures and faster wind speeds. Lower density
newly-fallen snow comes with colder temperatures and slower
wind speeds.
Snow density and ski quality
In skiing and avalanche science, a popular convention is to
represent snow density by its percentage of water and ice content,
called total water content. (Note: this
assumes that the densities of ice and liquid water are equal, which
is not true, but they are close enough) To convert from density in
terms of kg/m3 to %-water content, just divide
by 10 and add a percent sign. Therefore, according to the above Table
7b.1, freshly-fallen
and new snow typically range from 5-20%.
Fig. 7b.2 - High-density
newly-fallen snow at Steven's Pass in the Cascade Mountains of
Washington, USA. (Credit: West)
In general, low- to medium-density (light) snow is more enjoyable to
ski in than
high-density (heavy) snow. The lighter, fluffier snow is easier to push
around with your skis, while heavier snow tends to take more effort to
muscle through. Lighter snow also tends to spray or billow up into the
air more as you ride through it, which adds to the powder skiing
sensation/enjoyment ...and equally important, looks
better in photos and video.
Newly-fallen snow that's about 7% total water content or less
would be considered light, low-density snow, and the average is about
8-11%. Snow that is 11% or more is considered heavy snow. If
you look at the average snow density across North America (in and out
of the mountains), it's about 8%. Remember that this all refers to
newly-fallen snow, before it has settled (or been compacted like in a
ski resort).
Fig. 7b.3 - A skier on Yak Peak in BC finds some
very
nice low-medium density powder (likely 7-8%). (Credit: West)
Powder snow is generally considered to be
unconsolidated
(not packed) snow that is low to medium density. In powder snow, when
you gain enough speed your skis/board start to "float"
on the snow (similar to a waterskier or surfer). The rider can then
weight and unweight
their skis/board from turn to turn, which gives a nice
floating-bouncing sensation.
This, combined with snow spraying up in your face, is the ultimate goal
of
powder seekers. In fact, skis have become much wider over the past 15
years
with the goal of making it easier for skiers to float in powder.
The optimum snow density for powder skiing is actually not the
lightest snow
possible, but rather snow that's around 8% total water content. This
medium-density
snow is still easy to ski and light to push around/through, but has
enough "body" to provide flotation. In very low-density snow (~5%)
skis/boards have more of tendency to push through the snow
instead of
floating on top of it. This is typical of the Rockies' snow climate
which
features relatively small new snow accumulations with cold
temperatures,
resulting in small amounts of low density snow. These conditions may
make
for good photos with snow billowing up around you, but your skis/board
will mostly be just riding on whatever snow surface is underneath
the newly fallen snow.
In Learning Goal 7c we'll take things a step further, looking at how
density changes within newly fallen snow affect skiing/riding
quality.
Fig. 7b.4 - A skier gets deep into some low-density
powder in Big Cottonwood Canyon, Utah, USA. This snow is likely 5-7%
total water content. (Credit: West)
Density and avalanche danger
Snow density is an indication of the strength
of the snowpack. In general, the more dense the snow, the stronger the
bonding between crystals. In newly-fallen snow, the crystals
are
usually still in a stellar-type form. Avalanche problems within
newly-fallen snow are often the result of density changes during a
storm. We'll talk about this more in Learning Goal 7c.
Bonding between crystals in newly-fallen snow is not as strong as that
between rounds,
no matter what temperature it falls at.
One exception to this is when snow is falling during strong
winds. When this occurs, crystals collide violently in the air, and get
blown across the ground, breaking off the crystal arms. When they
settle on the ground they can become further packed by the wind. The
resulting newly-fallen snow can be very dense and well-bonded. This is
called wind board or a wind slab.
Fig. 7b.5 - Wind-packed snow on Mount Hood, Oregon,
USA. This would be considered wind board or wind slab. The weird
texture and ridges of the wind-affected surface is called sastrugi.
(Credit: West)
As we discuss in Learning Goal 7f, an unstable snowpack typically
results from denser layers overlying less-dense layers. Thus if you
have relatively high density newly-fallen snow (resulting from warm
temperatures or wind) that has fallen on top of a faceted layer, this
can result in an unstable, dangerous snowpack. Likewise, even
low-medium density newly-fallen snow, falling on top of
avery-low-density layer of surface hoar, can result in an unstable
configuration.
Keywords: newly-fallen snow density,
sastrugi, snow density, strength, wind board, wind slab
Figure Credits
Howard: Rosie Howard
West: Greg West
Stull: Roland Stull
COMET/UCAR: The source of this material is the
COMET® Website at http://meted.ucar.edu/ of the University Corporation
for Atmospheric Research (UCAR), sponsored in part through cooperative
agreement(s) with the National Oceanic and Atmospheric Administration
(NOAA), U.S. Department of Commerce (DOC). ©1997-2016 University
Corporation for Atmospheric Research. All Rights Reserved.
NOAA: www.nws.noaa.gov
Google: Map data (c) 2016 Google
Wagner: Wendy Wagner, Chugach National Forest
Avalanche Information Centre