What happens when a wind hits a barrier like a mountain
When a wind hits a barrier like a mountain, the air flow is disrupted and forced to rise, creating a phenomenon known as orographic lift. As the air is forced to rise, it cools and condenses, leading to the formation of clouds and potentially precipitation on the windward side of the mountain. On the leeward side of the mountain, the air descends and warms, creating dry and potentially warmer conditions, known as a rain shadow effect.
The interaction between the wind and the mountain can also lead to turbulence and gusty winds on both sides of the mountain, as the air is forced to navigate around and over the obstacle. Additionally, the wind can be funneled and accelerated as it passes through gaps or valleys in the mountain, resulting in stronger and potentially more destructive winds in these areas.