Futhermore, the World Meteorological Association posts Antarctic Ozone Bulletins in PDF format every two weeks. Visit their site for an in-depth overview of the Antarctic climate and ozone depletion. They also have a video regarding 2010 ozone and temp. datasheets here.
Ozone is O3 and when UV radiation strikes an O3 molecule it is photodissociated into O2 + O. Anthropogenic chemicals (CFCs and CFHCs) enter the atmosphere via pollution (i.e., freon leak from a car and then evaporated) and get broken down by atmospheric chemical processes. The result is single molecules are formed from the breaking down of CFCS, like chlorine. Chlorine destroys the drifting single O molecule, thus O2 + O cannot combine again to create O3. This process is more or less the removal of O molecules such that O3 cannot be recreated in the atmopshere.
Ozone depleting processes involve chemicals, temperature, polar clouds and sunlight. A good overview can be found here. Since there is now sunlight in the sky at Pole, UV radiation is bombarding the stratosphere. UV radiation is absorbed by the O3 in the stratosphere, the O3 molecules split, and since the number one rule of nature is energy in = energy out, that UV radiation is not lost but becomes thermal energy. The thermal energy radiated from the photodissociation of O3 heats up the stratosphere. This has a further impact on the creation of polar stratospheric clouds that correlate to the amount of ozone lost. These clouds create a surface (friction) by which molecules and chemicals collide, and they only occur when the stratosphere temperatures are just right.
The first two charts display only a slight disturbance in O3 concentrations in the stratosphere, probably due to air parcels from the outer bands of the vortex that moved into the interior of Antarctica and have already been undergoing ozone depletion associated with the impact of early summer UV radiation at higher polar latitudes.
And here is our most recent chart. Note that tempearture increased slightly at 15 km and that's where the ozone concentrations decline. This was our first distinct observation of the 2010 ozone hole.
Everything was fine relatively okay until about the 1960's. After that, the ozone hole began as the production of CFCs by industrialized and 'non-developed' countries sky-rocketed.
Over the course of a year, CFCs drift southward over the Antarctic winter-time. A continent-wide westard wind vortex encircles the South Pole right before twilight begins (June-July), it traps air molecules and chemicals. It's a caged witches brew just waiting for the UV radiation. When the sun arrives the party begins and ozone is removed from the atmosphere. There's a time towards the end of the Antarctic summer when the stratosphere becomes so depleted of O3 that the ozone-depleting chemical reactions slow down. By then winter is upon us again and the circumpolar vortex collapses and allows the passage of air between the high- and low-latitudes. More ozone 'flies' in to replenish the lost stock of ozone when the vortex is broken and UV radiation also disappears then, putting an end to the photodissociation of O3. Thus a rebound of O3. Think of it this way... O3 and CFCs and UV and SPC are put in a cage together for a few months, the result being O3 is removed from the atmosphere. Then the cage is lifted in Dec. and new O3 from the North is allowed to enter the space (along with more CFCs). This means that the global ozone budget is decreased every year.
How long will this keep going on? Whenever the ozone depleting molecules quit finding their way into the Antarctic vortex.
What's this mean for Polies? Wear sunscreen and sunglasses.