In most cases, the weather of the Leeward and Windward faces fluctuates in hot weather.
<h3>What is Leeward and Windward weather? </h3>
Mountain tiers act as boundaries to the drift of air throughout the floor of the earth.
When a parcel of hot air travels from a low valley to the foothills of a mountain range, it's far more pressured to make an upward push alongside the slope of the mountain because it encounters better terrain.
Opposite to the windward facet is the lee facet—the facet sheltered from the winning wind.
Because winning winds in the mid-latitudes blow from the west, this is frequently the Japanese facet of the mountain variety, but this isn't always the case.
Learn more about Leeward and Windward climate, refer to:
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