Ozone depletions in the lower stratosphere outside of polar regions ar
e difficult to explain using only local chlorine and bromine chemistry
. We speculate that iodine chemistry in combination with trends in ant
hropogenic chlorine and bromine may also be a factor in determining th
e widespread current depletion of lower stratospheric ozone. We also s
peculate on a related role for iodine in the sudden springtime surface
ozone loss observed in the Arctic.