When all layers of the snowpack are at the same temperature, typically at the freezing point. Often refers to a snowpack that is wet throughout its depth.
Condition that occurs in the the spring or after many cycles of melting and freezing.
When all layers of the snowpack are at the same temperature, typically at the freezing point. Often refers to a snowpack that is wet throughout its depth.
Condition that occurs in the the spring or after many cycles of melting and freezing.