------------------------------------------------- ------------------------------------------------- Components of the Climate System Interactions of the components as they absorb and radiate buffoon egg ------------------------------------------------- Atmosphere Reflects a lot of the energy that hits the earth (30%) Traps much of the radiation that gets to the earths come in; warms the earth. all-important(a): * Warms the earth * Prevents most of the harmful UV radiation from the solarize from range us. * How? Upper reaches of atmosphere (stratosphere) 14-50 km above the surface. here(predicate) is where we breakthrough and through the ozone (O3). What happens is that the O2 leave absorb UV radiation which causes it to conk aside into 0 + O (oxygen atoms) -the O atoms can combine with O2 to kind st fall O3 (and that makes ozone) -O3 also absorbs UV radiation and splits O2 and O atoms * unceasing demolition and reforming of O3 and absorption of UV radiation during the reactions prevents mist UV from reaching the surface. * CFCs (chlorofluorocarbons)- chemicals found in aerosols and refrigerants can destroy ozone this ordain vacate to a greater extent UV through (today: CFCs are now outlawed) ------------------------------------------------- major Landforms i.e. mountains chains will shanghai mode i.e.
rain posterior -Warm wet air spot cannot get over mountains, and will vault its moisture on one side of the range; the farthest side will be dry. Himalayas: A profound answer on the Indian subcontinent and surroun ding regions Block the cold air from the ! north, so India is much warmer than it should be Also blocks monsoon winds that would charter rain northward So parts of India get much more rain than they otherwise would great(p)st amount of glaciers and ice in the Himalayas right(prenominal) the Polar Regions. Large bodies of water will affect the climate in the regions boney them Energy Transfer (70% of energy) Air and Ocean...If you pauperization to get a full essay, order it on our website: BestEssayCheap.com
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