The breeze is a type of local wind driven by the movement of air masses due to the heterogeneous heating of relief by the Sun This leads to the occurrence of vertical movements of air masses that cause gaps and pressure imbalances. To restore these instabilities, new air masses moving to fill these gaps of low pressure. We distinguish the following types of breezes. Sea breezes. Located on the coast and are produced by the effect of differences in heating and cooling of the earth and water bodies. During the day the highest temperature of the earth gives rise to heated air ancestries that are quickly offset by the arrival of cold air from the sea or large lakes. In the evening there is a period of calm when the temperatures are equal. At night, the mechanism is reversed to be the hottest water but the wind speed is usually lower because the differences are not as pronounced. The southwest monsoon Asia are but a sea breeze and land a large scale in the season. Sea breezes deflected by the Coriolis effect tend to become virtually parallel to the coast with sustained winds and 2 to 7 m / s. Brisas valley and mountains. Similar to the previous result from the difference of heat stroke and differences in heating the air in the areas of peaks, valleys and headwaters of the funds themselves. This results in during the day there is a strong influence over sun-exposed slopes, and subsidence in the central part of the valley. Late in the day the opposite occurs, ie from the slopes, which are no longer heated by the sun, cooling the air descends toward the valley floor by lifting the warm air still remains in them. Text is available under the Creative Commons Attribution ShareAlike 3.0, additional terms may apply. See Terms of Use for more information.

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