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took effect and the amount of chlorine in the stratosphere decreased. In the Southern Hemisphere’s mid-latitudes, total ozone remained constant over that time period. There are no significant trends in the tropics, largely because halogen-containing compounds have not had time to break down and release chlorine and bromine atoms at tropical latitudes. Regarding ozone depleting substances , most are also strong greenhouse gases and, in a world without the Montreal Protocol on ODS ban minus 98% consumption worldwide between 1986 and restrictions, annual ODS emissions could be today as important for climate forcing as those of CO2 and be 10-fold larger than its present value Transitory ODS substitute gases, H-CFCs first, then HFCs are also greenhouse gases but most of them to a lesser extent and their transitory use as substitutes to ODS represented the most important contribution to the reduction of the global greenhouse gases emissions. In the 1970’s it was discovered that every spring, a “hole” was formed in the stratospheric ozone layer in particular over Antarctica, and that some chemicals made by humans were responsible of the destruction of ozone. The very low winter temperatures in the Antarctic stratospherecause polar stratospheric clouds which temporarily prevent “fresh ozone” produced in the tropical region to replace the destroyed ozone. The reduction of the ozone layer changes the UV-radiationreaching the earth surface and this has various impacts on the environment, on health. Most ozone depleting substances are also strong greenhouse gases and, in a world without the Montreal Protocol on ODS ban minus 98% consumption worldwide between 1986 and restrictions, annual ODS emissions could be today as important for climate forcing as those of CO2 and be 10-fold larger than its present value Transitory ODS substitute gases, H-CFCs first, then HFCs are also greenhouse gases but most of them to a lesser extent and their transitory use as substitutes to ODS represented the most important contribution to the reduction of the global greenhouse gases emissions. As a result of the success of the Montreal Protocol in limiting ozone depletion, since the mid-1990s the changes in UV-B measured at many sites are due largely to factors other than ozone. Nevertheless stabilisation of the concentrations of stratospheric ozone and possible beginning of a recovery of UV-B irradiance are not yet detectable in the measurements because of the large natural variability. The distribution of total ozone over Earth varies with location on timescales that range from daily to seasonal. Total ozone is generally lowest at the equator where it is produced and highest in polar region atmosphere. The variations are caused by large-scale movements of stratospheric air and the chemical production and destruction of ozone. An important feature of seasonal ozone changes is the natural chemical destruction that occurs when daylight is

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