The layer of the atmosphere that is above the troposphere, whereC-Cl bondsin CFCs arebrokenin UV radiation to formchlorine radicalswhichcatalysethebreakdown of ozone
The lowest layer of Earth's atmosphere, by which point most of the high energy UV has alreadybeen absorbedin the ozone layer, meaningless CFC breakdown
A substance thatincreases the rateof a chemical reaction by providing analternative reaction pathwaywith alower activation energy, whilst remainingchemically unchangeditself
Havetwoactivation energies (adouble humpin the diagram, with thesecond one lowerbut both smaller than with no catalyst) where theintermediatesare formed in the centre
Energy the Earth absorbs from the sun isre-emittedmainly asinfra-red(at a lower frequency than that of the sun) andtrappedin the atmosphere by the ozone layer
The constant in a reversible reaction that is specific for a certain temperature (increases when to right/decreases when to left) but is not affected by a change in concentration