Less ozone above the tropopause causes less stratospheric warming, allowing the tropopause up, which pushes the climate zones towards the equator.
Not exact matches
In addition, the larger than expected loss of UV light meant
less stratospheric
ozone up to 45 kilometers
above the surface, but more
above that line.
Less intense depletion of
ozone occurs
above the Arctic and in mid-latitudes of both hemispheres.
Low solar activity sees the atmosphere
above the South Pole cool both directly with
less solar radiant energy and as reduced
ozone warming by solar ultraviolet radiation.
When the Sun is more active there is more
ozone above the equator and
less over the poles, and vice versa.