When WRF is used for extreme precipitation simulation why does the height of Windward slope Mountain increase and the precipitation of Windward slope decrease

This is because in extreme precipitation events, the atmosphere becomes saturated with moisture, and the air rises rapidly. As the air rises up the windward slope of a mountain, it cools and condenses, leading to precipitation. However, if the precipitation is too extreme, the rising air may not be able to reach the top of the mountain and instead gets blocked by the height of the mountain, leading to a decrease in precipitation on the windward slope. Additionally, the rising air may also cause the mountain to have an increased height due to the uplift of the rock layers