Sea breezes punch from the cooler s over the warmer land in summer. Sea breezes punch at about 10 to 20 km (6 come 12 miles) per hour and also lower air temperature lot as 5 come 10oC
Land breezes punch from the land come the sea in winter. Some warmer waiting from the s rises and also then sinks on land, causing the temperature over the floor to come to be warmer.

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Monsoon winds are larger scale versions of land and also sea breezes; they blow from the sea ~ above the floor in summer and from the land onto the sea in winter. Monsoon winds happen where an extremely hot summer soil are beside the sea. Thunderstorms are usual during monsoons.
Temperature differences in between mountains and also valleys develop mountain and also valley breezes. Throughout the day, wait on hill slopes is heated an ext than air at the same elevation over an surrounding valley. Together the work progresses, warmth air rises and draws the cool air up from the valley, producing a sink breeze.
At night the hill slopes cool more quickly 보다 the nearby valley, which reasons a hill breeze to flow downhill.
Katabatic winds move up and down slopes, but they room stronger mountain and valley breezes. Katabatic winds kind over a high land area, choose a high plateau. The plateau is commonly surrounded on virtually all sides by mountains.
Chinook winds (or Foehn winds) develop when wait is required up over a hill range. This take away place, because that example, once the westerly winds bring air native the Pacific s over the Sierra Nevada mountains in California.
Snow top top the leeward next of the mountain melts quickly. If precipitation falls as the waiting rises end the mountains, the air will be dry as it sink on the leeward size. This dry, sinking air causes a rainshadow impact which creates countless of the world"s deserts.
Santa Ana winds are developed in the late fall and also winter once the an excellent Basin east of the Sierra Nevada cools, producing a high push zone. The high pressure pressures winds downhill and in a clockwise direction.

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High summer temperatures on the desert create high winds, which are often associated with monsoon storms. Desert winds choose up dust due to the fact that there is not as lot vegetation to hold down the dirt and also sand. A haboob develops in the downdrafts on the front of a thunderstorm.
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