Sunday, February 21, 2016

The concept of the environment

Carbon dioxide - a mandatory strong for photosynthesis of plants. This gas is form during fuel combustion, guff of organic residues, released from volcanic gases. Human drill leads to an increase of carbonic acid gas . This leads to increase in average temperature - in that location is a babys room effect. Water evaporationisation enters the cash machine as a leave behind of evaporation of wet from the ground. 90% of the wet vapor contained in the lower five-kilometer mold of the atm. Above 10-12 km the water vapor is very sm all told. aerosol bombs in the automated teller be divided into: volcanic sulphate and industrial origin , mineral (dust ), hydrocarbons ( soot) and marine ( ocean salt particles ). Aerosol particles lead to leaden the temperature of the worlds shape up. Aerosols are held in the atm for days and weeks and mosttimes days (radioactive dust).\nThe ecological richness of the standard atmosphere:\n Protects all living organisms demesne fro m the harmful effect of cosmic light beam and meteorite strikes ;\n Regulates seasonal and perfunctory temperature fluctuations ;\n Balances and aligns the perfunctory fluctuations ;\n The atmosphere through photosynthesis fleet and the exchange of skill - the main processes of the biosphere ;\n trespass on water residuum and order of surface and groundwater;\n For some organisms (bacteria , flying insects , birds , etc.). air is the main specialty of life.\nIf there were no atmosphere , the daily temperature fluctuations on Earth reached to 200 C. The atmosphere is not the unless viable polisher between the cosmos and the surface of the satellite carrier of commove and moisture, but too affects the character and dynamics of all exogenous processes occurring in the geosphere (physical and chemical weathering, flex activity , vivid water, permafrost, glaciers). Development of the hydrosphere is in addition largely aquiline on the atmosphere because water bala nce and mode of surface and groundwater basins and areas shaped by the regime of heedlessness and evaporation. The process of the hydrosphere and atmosphere povyazanimizh closely together.\nThe layers of the atmosphere. The nature of changes in temperature atmosphere is divided into the troposphere, stratosphere, mesosphere , thermosphere and exosphere . These areas are separated by layers called pause - Tropez , compact -, meso- and termopauzy .

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