Snow Conditions
Powder
Snow forms when water vapours rise into the atmosphere to form clouds. With enough moisture and the temperature at or below freezing they will begin to form ice crystals. As they accumulate and become heavier they will start to fall and combine to make flakes that land on the ground. When enough of this beautiful, white fluffy snow gathers over a short period of time there will be powder snow. The temperature at which the snow formed, fell through the air and accumulated at the ground, the humidity, wind direction and strength as well as the aspect of the terrain will all influence the snow’s quality.
People will usually be very excited about fresh snow and decision making is often clouded. Space students out to avoid collisions. Snow being sprayed, although fun, can create total blindness for brief periods of time. Consider riding a directional, powder board specifically designed for riding deep, soft snow. Identify flat spots as speed will need to be carried through these sections. Use other riders’ and skiers’ tracks to keep speed through flat run outs.
Crud
Crud is formed through the combination of snow, wind, sun, rain and tracks left in the snow. Crud will often offer up a true mixed bag of conditions, the top section on a slope might be icy and wind blown, followed by some punchy, crusted snow with powder underneath and finishing in some untracked, soft snow.
Slush
When the air temperature warms beyond freezing point, the delicate snow crystals melt causing an increase in the water content of the snowpack, transforming the snow into larger grains of ice and slush is formed. Slush will change rapidly due to temperature fluctuations and often occurs in spring when the winter snowpack begins to melt. Warmer slush is deeper and often sticky, especially if it is new snow transitioning to slush. Cold slush is firmer and faster. Once the snow pack starts to melt and then refreeze it will often be icy in the morning and become slushier as the day warms.
Ice
Characterised as being firm, shiny, slick and loud when riding, icy snow can be encountered in every resort around the world. When snow begins melting and the snow structure breaks down, the water content in the snowpack increases. If this is followed by a period of freezing temperatures, the snowpack will become a more solid surface and form ice. It can be found following long periods without snow, heavy traffic on the snowpack as well as during the spring time following the often daily freeze/thaw cycles.
Some things to consider when riding and teaching students on icy terrain. Stopping points should be on areas that students can safely stop without sliding or being slid into. Understanding of the individual’s skill and confidence level must be carefully assessed. Students who were once comfortable on a nice groomed run with soft snow may become nervous once the snow hardens up. Fear can often arise due to the lack of control, noise and feeling as well as falls being more painful due to the hard nature.
Due to ice being so dense the snowboard’s edge has difficulty connecting with the snow. Therefore, balancing on an edge and staying in control becomes increasingly difficult. Being able to ride it efficiently involves using progressive lateral movements through the lower body with more of a rotational and steering focus to control speed.