wildwohl said:
Who is making ozone to fill in the hole?
Not who, but what. It's sunlight.
Sunlight can photolyze ordinary oxygen molecules (O
2), creating a pair of oxygen atoms. This is a fairly slow chemical process. A collision between one of those free oxygen atoms and another O
2 can create ozone. This is a fairly fast chemical process. Sunlight can also photolyze an ozone molecule, splitting it into an O
2 molecule and a free oxygen atom. This is also a fairly fast chemical process. (Note: This is also the process that protects us from ultraviolet radiation.) That free oxygen atom won't last long; it will either collide with an O
2 molecule to create a new O
3 molecule (fast), or it will collide with an O
3 molecule to create a pair of O
2 molecules (slow). Ozone can also spontaneously split into O
2+O, but this is quite slow.
Summary so far: With sunlight, a number of chemical processes of varying speeds work together to make for an equilibrium distribution of oxygen in the form of oxygen atoms, O
2 molecules, and O
3 molecules. So what happens without sunlight? Now the processes favors ordinary oxygen as opposed to ozone. There is a natural depletion rate of ozone during winter.
So far I've only talked about oxygen and sunlight. Ozone is highly reactive. Add something to the mix with which oxygen can react, in general ozone will do it best. Foreign substances act to alter the mix of O versus O
2 versus O
3. These foreign substances act as a sink for ozone. The consequences of those foreign substances will have limited scope if the reaction in question is a typical chemical reaction. The consequences are much more severe if the reaction is catalytic, and that is exactly what happens in the case of the chlorofluorocarbons. The problem is greatly exacerbated in winter, where there is essentially no sunlight to create new ozone molecules.