Natural reasons:
There is a long period of low temperatures ( below 78° C ) over Antarctic in the spring, which causes a vital process. It is the polar air sinks by the cold that forms a strong westward circulation called the "polar vortex". Its major role is to isolate the Antarctic air from the rest of the atmosphere, making the atmosphere inside the vortex a giant reactor. Low temperature conditions can also help ice cloud or liquid aerosols to absorb atmospheric pollutants. Thus the sunlight is able to activate those pollutants especially chlorine and bromine, which increases ozone consumption (the chemical process refers to last post).
There are other three theoretical explanations for the formation mechanism of ozone hole: (1) the changes in polar meridional circulation cause the ozone transported to the Antarctic to decrease and form an ozone hole; (2) the heterogeneous chemical reaction under the polar ice crystal effect causes ozone reduction; (3) the combined effect of the dynamic meteorological factors and photochemical reactions related to solar radiation causes the formation of the ozone hole.
Anthropogenic reasons:
Synthetic chlorine and bromine-containing substances are
responsible for the Antarctic ozone hole, most notably CFCs (CFCs) and bromine
compounds (Halon). Molecules of CFC and Halon released by humans are heavier
than air molecules, but they are chemically inert in the troposphere.
Even the most active atmospheric component, the oxidation of free radicals to
CFC and Halon, is negligible. Therefore, they are very stable in the
troposphere which can not be removed by normal atmospheric chemical
reactions. Over the course of a year or two, these compounds are distributed
evenly across the troposphere in the world and mainly brought into the
stratosphere by the atmospheric circulation over the tropics, which in turn
transports them from low latitudes to high latitudes, with layer
being evenly mixed. In the stratosphere, intense UV radiation
causes dissociation of CFC and Halon molecules, releasing highly reactive
atomic states of chlorine and bromine which are also free radicals. Chlorine
radicals and bromine radicals are the main substances destroying
the ozone layer which is catalyzed, so do Bromine radicals. It has been estimated
that one chlorine atom radical will destroy 104-105 ozone molecules while the
bromine atom radical released by Halon has 30-60 times as much destruction of
ozone as chlorine atoms. In addition, there is a synergistic effect between
chlorine atom radicals and bromine radical radicals. In other words,
when both of them are present at the same time, the ability to destroy
ozone is greater than the simple summation of the two.
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