Recently, additional ozone production mechanisms have been proposed to resolve the ozone deficit problem, which arises from
greater ozone destruction than production in several photochemical models of the upper stratosphere and lower mesosphere.
Not exact matches
The formation of large areas of high pressure in the lower atmosphere both lowers
ozone levels, by squeezing the
ozone layer above, and may provide the very cold conditions in which
ozone destruction is
greatest.
The
greatest ozone density is around 20 - 25 km because the
ozone destruction processes are slower there.