Which side of the mountain typically experiences more snow and less wind?

The leeward side of a mountain typically experiences more snow and less wind due to a weather phenomenon known as orographic lift. When moist air approaches a mountain range, it is forced to rise over the peaks. As the air ascends, it cools, causing moisture to condense and precipitate as snow or rain on the windward side of the mountain. This results in heavy precipitation on the windward side.

Once the air crosses the peak and descends on the leeward side, it warms and dries out, leading to drier conditions and reduced snowfall, this area is often referred to as a rain shadow. Consequently, the leeward side experiences significantly less wind because the force of the wind is interrupted by the mountain's presence, creating calmer conditions compared to the windward side, where strong winds are common as they push against the terrain.

This explanation highlights why the leeward side is more apt to have greater snowfall accumulation and a generally calmer wind environment.