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Land Breezes, Sea Land Breezes, Sea Breezes and Rain Breezes and Rain Shadows Shadows

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Land Breeze and Sea Breeze

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  • Land Breezes, Sea Breezes and Rain Shadows

  • OBJECTIVEDiferenciar cada componente que hace parte del ciclo del agua para comprender cmo podran ser afectados por el relieve y las condiciones climticas presentes en el planeta Tierra.

  • LEARNING OBJECTIVEComprende cmo las corrientes de aire, la temperatura y el relieve determinan el ciclo del agua para establecer cunto influyen a travs de instrumentos para medir el clima.BIBLICAL PRINCIPLE:Ecclesiastes 1:6The wind blows to the south and turns to the north; round and round it goes, ever returning on its course.

  • Sea Breeze

  • During the day, the land warms up faster than the water. The sea breezes move from water to the land.

  • SEA BREEZE

  • Land Breeze

  • Land Breeze:At night, dry land cools faster than water, due to the waters large specific heat capacity. The breeze moves from the land to the water.

  • RAIN SHADOWSArain shadowis a patch of land that has been forced to become adesertbecause mountain ranges blocked all plant-growing, rainyweather. On one side of the mountain, wet weather systems drop rain andsnow. On the other side of the mountainthe rain shadow sideall thatprecipitationis blocked

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