ozone

                                                  

                                        
                                               Same CO2 radiative forcing of global surface temperature is expected to cool the stratosphere.  by cooling turuvaocon (O3) is an increase in the lesion.  ozone holes.
    Ozone depletion represents a radiative forcing of the climate system. The two opposing effects: Reduced ozone layer vantalam absorb less solar radiation. The stratosphere is cooling. Troposphere warms as a result of colder stratosphere stratosphere, releasing less long wave radiation. Thus, cooling troposphere. Cold there is widespread; IPCC, "In the past twenty years, observed stratospheric O3 losses poricinkai negative surface troposphere system.", He said. ( -0.15 ± 0.10 watts for a ckuver meter (W / m²)).
    Greenhouse strongest predictions of the stratosphere will cool as a very clear contracts.  Greenhouse valimankalinalum ozone citaivinalum condensation occurs because both the effect of the changes we . The stratospheric numerical done by. National Oceanic and Atmospheric Administration's Geophysical Fluid Dynamics laparatori from the published study results, 20 km (12.4 miles) above, deals with the greenhouse gases that can easily show that the cooling process.
    Ozone depleting chemicals are also greenhouse gases. Increase in chemicals, 0.34 ± 0.03 W / m² radiative creditable amount. Well-mixed greenhouse gases increases in the total represents a radiative forcing caused by the 14%.
    This long term process. Its measurement, research and theory into global ataravaipperru, hypothesized in the dominant ozone citaivaipparriya .1980 s theories, published in 1990. They are still being proven. Dr Drew Schindell, Dr Paul Newman, NASA Goddard, 1990 proposed a concept of. SGI Origin 2000 supercomputer using computers it was pativattukkul ozone destruction system. 78% of the theory of ozone destroyed. Further refinement of this principle, it Ozone alivaikkattiyatu 89%. Putupittu is to come back 75 years that ozone is an account that pushed back 150 years. (The most important aspect is that this form in the stratosphere comes from the bones of fuels is the fly)