This paper develops a new theory of
stratospheric ozone formation in situ at high latitudes, based upon tropospheric transport and conversion of paramagnetic oxygen.
Not exact matches
In September, the
ozone hole is at its largest because the cold winter months coupled with the returning daylight permit
stratospheric cloud
formations that do the most damage to the
ozone layer.
(Such low air temperatures encourage the
formation of icy clouds in the upper atmosphere known as polar
stratospheric clouds, which foster the chemical reactions that turn harmless chlorine compounds into
ozone eradicators.)
Aircraft emissions probably play a crucial role in
ozone destruction by fuelling the
formation of polar
stratospheric clouds.
This could enhance the
formation of polar
stratospheric clouds, which convert potential
ozone - depleting species to their active forms.
In an idealized three - dimensional numerical simulation of the Northern Hemisphere winter stratosphere, doubling the CO2 concentration leads to the
formation of an Arctic
ozone hole comparable to that observed over Antarctica, with nearly 100 % local depletion of lower -
stratospheric ozone.