Unit IX: Ozone

Ozone (O3) is a gaseous molecule composed of three oxygen atoms.
90% of the atmospheric ozone resides in the stratosphere between 10
and 50 km.
1. An ozone molecule is formed when UV radiation at very short
wavelengths (<200 nm) breaks an O2 molecule into two oxygen atoms.
These oxygen atoms (O) then react with other oxygen molecules (O2) to
form ozone (O + O2
2. Ozone is broken apart by the Sun's ultraviolet radiation at a longer
wave lengths (200 to 300 nm) into an oxygen molecule (O2) and an
oxygen atom (O). The oxygen atom can then react with another O2
molecule to reform ozone. This cycling of ozone to oxygen atoms and
back to ozone consumes the UV radiation and converts it to heat.
3. Ozone can also be destroyed when the Sun’s UV radiation breaks
ozone into an oxygen molecule (O2) and an oxygen atom (O) and the
oxygen atom recombines with another oxygen atom to form a molecule
of O2.
4. UVC (200-280 nm) radiation can break the chemical bonds in DNA
molecules. UVB (280-320 nm) radiation is largely responsible for skin
cancers and eye damage. Fortunately, ozone absorbs all UVC and 90%
of the Sun’s UVB radiation. Ozone is not effective in screening UVA
(320-400 nm) which mostly tans us. We are concerned about ozone loss
because without it, highly damaging UV radiation would reach the
Earth’s surface, putting all life forms are risk.
5. Ozone is also destroyed by catalytic processes, wherein the ozone
molecule is lost (converted to molecular O2), while the catalyst
(chlorine, nitrogen, bromine or hydrogen) is released unchanged to
destroy another ozone molecule.
6. Long-lived trace gases such as CFCs are lofted into the stratosphere
from the tropical upper troposphere. After entering the stratosphere, the
CFCs are typically transported into the midlatitudes and carried back out
of the stratosphere. A small fraction of the CFCs are lofted into the
upper stratosphere (above the ozone layer), where they are broken up by
the Sun's extreme shortwave UV radiation, releasing the chlorine atoms
that act as catalysts that cause ozone destruction.
7. The Antarctic ozone hole is directly a result of the human produced
Chlorine-compounds that enter the stratosphere (principally CFCs). The
hole appears each spring in the southern hemisphere (AugustNovember) over Antarctica following the extremely cold Antarctic
winter. The hole results from chemical reactions that occur on the
surface of polar stratospheric cloud (PSC) particles. These special
reactions release chlorine from benign forms (HCl and ClONO2) into a
form that can quickly catalytically destroy ozone.
8. Compounds such as CFCs that can cause ozone loss have now been
regulated by international agreement. Chlorine compounds that can
destroy ozone have begun to decrease in the lower atmosphere and are
expected to start to decrease soon in the stratosphere, although their long
residence times (decades to centuries) means it will be 50 years or more
before ozone returns to its pre-industrial level. Future impacts on the
stratosphere from aircraft and greenhouse gas effects are currently under
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