33 OZONE DEPLETION IN THE STRATOSPHERE
Less ozone in the stratosphere allows for more harmful UV radiation to reach the earth's surface.
Not exact matches
One driver of temperatures
in this region is the abundance and variability of
ozone, but water vapor, volcanic aerosols, and dynamical changes such as the Quasi - Biennial Oscillation (QBO) are also significant; anthropogenic increases
in other greenhouse gases such as carbon dioxide play a
lesser but significant role
in the lower
stratosphere.
The various kinds of evidence examined by the panel suggest that the troposphere actually may have warmed much
less rapidly than the surface from 1979 into the late 1990s, due both to natural causes (e.g., the sequence of volcanic eruptions that occurred within this particular 20 - year period) and human activities (e.g., the cooling of the upper part of the troposphere resulting from
ozone depletion
in the
stratosphere).
Another pathway even
less studied is caused by the energetic particle rain at polar regions, where HOₓ and NOₓ chemical species are created
in the polar regions of the thermosphere and mesosphere and transported down to the
stratosphere where they destroy
ozone.
You introduced
ozone in an attempt to explain away the inconvenient fact that the
stratosphere cooled when the sun was more active and is now warming whilst the sun is
less active.