How are mountain and valley breezes formed? Suppose there are two mountains. Class 9
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How are mountain and valley breezes formed? Suppose there are two mountains. Class 9
Question 1.
How are mountain and valley breezes formed? Suppose there are two mountains, one covered with grass and another covered with barren rocks; would the temperature of the two mountain breezes be different? If so, how? Class 9
Answer:
Formation of Valley Breeze (Daytime):
- During the day, mountain slopes facing the Sun heat up more rapidly than the valley floor.
- The air over the slopes becomes warm and rises, creating a low pressure region on the slopes.
- Cooler air from the valley moves upward toward the slopes to replace the rising warm air.
- This upward flow of cool air from valley to slopes is called the valley breeze.
Formation of Mountain Breeze (Nighttime):
- After sunset, mountain slopes lose heat faster than the valley floor.
- The air over the slopes becomes cool, dense and heavy, and flows downward into the valley.
- The valley floor remains relatively warmer compared to the slopes.
- This downward flow of cool air from slopes to valley is called the mountain breeze.
Such breezes are commonly experienced in hilly regions like Shimla, Dehradun and other Himalayan valleys.