The most common form of hoarfrost is called surface hoar. This consists of ice crystals that form on top of snow banks, usually overnight. The sparkles you see coming from a field of snow are often reflections off the facets of surface hoar crystals.
Surface hoar typically forms when a snowbank warms up during the day and is then cooled again overnight. The night air cools the surface of the snowbank more than the inside, so that water can evaporate from inside the snowbank and recrystalize on the surface. By morning the snowbank is covered with a layer of faceted ice crystals, and they can be quite large. These usually melt again once the sun comes up, so the best time to find surface hoar is early in the morning.
or click
Heads or Tails.
Thank you so much for visiting.
Thank you so much for visiting.
Technorati Tags: surface hoar, snowcrystals.com, hoarfrost, Heads or Tails, Missisquoi River, January thaw
_/\_/\_
_/\_/\_

