6 characteristics of valley winds
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The warmer and less dense air near the ground rises during the day pulling more air through the valley floor. This gentle upslope wind known as a valley breeze. The flow of air reverses as the sun is going down and at night. This is because the mountain slopes at higher elevations cool quicker than the valleys.
They are not the same as katabatic winds, which are larger and stronger. These winds are opposite from each other. While valley breezes occur when the warm air rises up the sides, warm air in a mountain breeze will rise up the middle. Mountain and valley breezes form through a process similar to sea and land breezes.
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