As the air mass reaches the other side of the lake, the engine of rising and cooling water vapor pans itself out in the form of condensation and falls as snow, usually within 40 kilometers of the lake.
The water vapor condenses and falls as snow, usually within 40 kilometers of the lake. As the air mass reaches the other side of the lake, the air rises and cools again.
As the air mass reaches the other side of the lake, the air rises and cools again. The water vapor condenses and falls as snow, usually within 40 kilometers of the lake.
As the air mass reaches the other side of the lake, the air rises and cools again. The water vapor condenses and falls as snow, usually within 40 kilometers of the lake.