qOther atmospheric trace constituents, such as
 nitrous oxide (N2O), water vapor, and freons, can also be photolyzed. They produce
 highly reactive radicals that keep ozone abundances lower than they would otherwise
 be.
 qThese radicals include: nitric oxide (NO), atomic
 chlorine (Cl), bromine (Br) radicals, and hydroxyl (OH) radicals.
 qThese radicals can destroy stratospheric ozone
 through “catalytic cycles”.