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Snow Has a Mind of Its Own
By Larry Olmsted
Trailside
Adapted from
Snowshoeing
by Larry Olmsted

Falling snow has widely varying characteristics based on moisture content. In addition, many changes occur—once snow lands on the ground savvy skiers rise at daybreak to hit the slopes after a new"dump" of powder, not only to beat other skiers, but time and Mother Nature, as well. They know that gravity pulls the snow toward the earth, compacting it and making it denser. Even in the untouched wilderness, powder becomes denser over time.

Montana's Big Mountain

Wind also plays an important role in packing the snow down and making it denser. In fact, in open, windswept areas, wind-packed snow can become so dense that Eskimos are able to cut blocks out of it and use them to build igloos.

Warmer temperatures generally make for firmer snow: the snow melts during the day and refreezes at night, becoming denser. On the other hand, snow in very cold, windless regions—like the forests of Minnesota, where the temperatures remain well below zero for weeks on end—will remain light.

Denser snow is better for snowshoeing, so welcome the sun, the wind, and time. If you are out West and get a big powder storm and find yourself unable to effectively move around on your snowshoes, just wait until it firms up a bit. This may take a few hours or a few days, depending on the conditions.


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[from Outside magazine]