These forms when air moves in the directions shown by the arrows in the diagram is the c. mountain breeze.
These winds are contrary from every other. Mountain winds blow from mountain closer to valley after sunset, while mountain cools down and valley quarter is relatively warmer. While valley breezes arise while the nice and cozy air rises up the perimeters of the valley, heat air in a mountain breeze will upward thrust up the middle.
Alternate titles: mountain wind. When the valley ground warms all through the day, heat air rises up the slopes of surrounding mountains and hills to create a valley breeze. At night, denser cool air slides down the slopes to settle withinside the valley, generating a mountain breeze.
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