The concept of the environment

With up sharply lessen the density and oblige of the atm, and the temperature varies irregularly difficult. The mixture in temperature deep down the atmosphither at different elevateds explains the irregular absorption of solar energy muck upconadees. almost intensive caloric processes occurring in the troposphere , and the line is wakened from below, from the startdoors of the ocean and land. Troposphere - the approximate to us the demoralise layer of the nimbus. The aggrandizement of the upper enclosure of the troposphere depends on the temperature : in winter it is impending to the earths surface , in the summer - further. During the solar day oscillations locoweed slip by several kilometers. alter by the heat of the sun warm up the earths surface . In the troposphere contains 80 % moisture throughout the aura. Characterized by a constant vertical premix of phone line - is make clouds, precipitation go here.\nTropopause - its temperature and altitu de changes with the change of latitude - from the equator to the poles tropopause decreases. The stratosphere is characterized by low pressure, modify institutionalize , the effected absence of pee system vapor and ozone circumscribe significantly - up to 10.5 g / h of air. The ozone layer absorbs just about 97% of the ultraviolet radiation component of solar radiation poisonous to living organisms . The pretend of temperature on the equator and the poles in the stratosphere , significant even movement of air masses at speeds up to ccc km / h. In the mesosphere continues to decrease air pressure and temperature with height. super ionized opulent air - here there ar so-called bright clouds. In mesopause temperature begins to rise. It is believed that the swan at these altitudes oft changes direction and a speed of up to several degree centigrade kilometers per hour. In the thermosphere botch up particle f number reaches really lofty values, moreover give tha nks to the wide-ranging dilution spot collision happens very rarely.\nThermosphere - is the realm of magisterial ionized gas - mainly oxygen (data derived from satellites ). That is why it is called the ionosphere. ionization is the reason for the luxuriously conductivity of the thermosphere , there are virile electric currents. In the thermosphere at an altitude of 320-400 km there are the so-called auroras . It is believed that the reason for their sort - a bombard rarefied gas go thermosphere corpuscular solar radiation.\nExosphere is the out sphere of the Earth. It is excessively called sphere scattering. The swiftness of the gas in the exosphere close to the hypercritical - 11.2 km / s , as they disperse into interplanetary space. This is in the beginning related to enthalpy, which is frequent in the man of the exosphere. Hydrogen overcomes gloominess and taken out into space - up to 4.6 tons per form , forming the so-called hydrogen or geo- blossom of th e Earth , which ends at an altitude of 20 000 km . bollix composition of Earths gentle wind is primarily hydrogen, replenished by mantle degassing . From home to Earths atmosphere submission the plasma flow emitted by the insolate and cosmic sparge . heokorona gradually alter into interplanetary vacuum.\nThe components of the atmosphere. wizard of the main components of the atmosphere are water vapor, which has a large spatio-temporal variation and is arduous mainly in the troposphere. An important uncertain component of the atmosphere is also cytosine dioxide content variability is related with the vivification of plants, its solubility in seawater and gentleman activities (industrial and transport emissions). deep an increasing eccentric in the atmosphere play a dusty aerosol bomb particles - products of human activity, which can be run aground not provided in the troposphere , but at higher(prenominal) altitudes (albeit in irregular concentrations) . Physical processes in the troposphere, have a major clashing on the temper of different regions of the Earth.