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1/21/2023
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eavatorial insulator polar insulation to a ialais jahon ack anright polar cetatorial insulation insulation effect of 90%. GOON archicl circle lines of latitude - arctic .3 cells polar, ferrel, hadley, hadley, ferrel, polar circle, tropic of cancer, equator, tropic of Capricorn, antarctic círcie Alobal circulation system 30° N FTOPIC OF cancer equator propic Of Capricorn 60°5 antarctic circle TAS DO 90%- stages of GCS : • air cools + sinks creating high pressure + cold dry climate - at about 60°N +Scold polar air mixes w/ warmer air t rises creating low pressure cool air sinks, creating hp, as air sinks it becomes warmer+drien warm air rises, creating lp. as air rise it cools - crouds form + release precipitation. , above the air with separare + more to higher latitudes suns heat is concentrated suns hear is spread out 30°5 heat from tropical to GS can be described as the worldwide systemor winds by which the Frans port of atmospheric circulation. the movement of air around to earth to try ★ balance temp polar cell Polarcell ferres cell the eavo than the poles the 1) Ferre) cell thadleycell Thadley cell Polar atitudes is solar radiation the Juns energy that reaches the earth J Poles are at air at the equator rises air at the poles falls warm air rises - low pressure cold air falls high pressure the equator is at 0° latitude accomplished 90° latitude receives more solar radiat; ocean currents are a major component in transferring heat energy. - warmourrents carry water. Poteward raise the air temps of the environments they flow e.g. me gulf stream cold currents canly water the equator + lower towards temps or coastal areas dig. the cangries. the main ocean currents follow...
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circular routes -clockwi se in nh, anti in sh - alocations proximity to the oceans can have a large impact on its climare be water can hold hear fora long time