Natural capital degradation: simplified summary of how chlorofluorocarbons (CFCs) and other chlorine - containing compounds can
destroy ozone in the stratosphere faster than it is formed.
Figure 20.18 Natural capital degradation: simplified summary of how chlorofluorocarbons (CFCs) and other chlorine - containing compounds can
destroy ozone in the stratosphere faster than it is formed.
Not exact matches
Thirty years ago, the Montreal Protocol was agreed to phase - out chemicals
destroying the
ozone layer, the UV - radiation shield
in the Earth's
stratosphere.
Ueno says that once aerosols are
in the
stratosphere they become very stable and can last for years, compared with days or weeks
in the troposphere, and they can activate compounds such as chlorine that
destroy the
ozone layer.
A 20 - year study by German scientists has found that the rate of increase of CFC - 12, a chlorofluorocarbon compound that spawns
ozone -
destroying reactions
in the
stratosphere, has slowed since 1990, although absolute levels are still rising.
«This is the only long - term data set with regular measurements of
ozone -
destroying compounds
in the
stratosphere,» says atmospheric chemist Darin Toohey of the University of California, Irvine.
Because they are released
in large quantities from tropical oceans, they are rapidly lofted by tropical thunderstorms into the
stratosphere within a month or two where they can
destroy ozone for a larger portion of their lifetimes.
No specific mention of the «volume cold enough for
ozone loss» trend line is made
in the Nature text, although it is stated that «Certain clouds
in the
stratosphere provide surfaces on which CFC decay products are converted into forms that
destroy ozone â??
Also, the overall number of
ozone molecules
destroyed in a vertical column of air was pretty much the same as the number of molecules transported into this column by the average poleward and downward transport of air
in the
stratosphere.
Although production of
ozone -
destroying gases has been curtailed under international agreements, concentrations of the gases
in the
stratosphere are only now reaching their peak.
By
destroying ozone (itself a greenhouse gas)
in the
stratosphere, CFCs also affect the climate indirectly
in ways that are still not fully understood.
On the other hand, CFCs
destroy ozone (a GHG)
in the
stratosphere.
«The rate at which
ozone is being
destroyed in the upper
stratosphere is slowing, and the levels of
ozone -
destroying chlorine
in that layer of the atmosphere have peaked and are going down»
The other is that very short - lived substances (VSLSs), which contain chlorine and bromine, could be
destroying ozone in the lower
stratosphere.
In 1974, Dr. Mario Molina and Dr. Sherwood Roland of the University of California published a paper asserting that chlorofluorocarbon (CFC) pollution from industry was destroying the ozone layer in Earth's stratospher
In 1974, Dr. Mario Molina and Dr. Sherwood Roland of the University of California published a paper asserting that chlorofluorocarbon (CFC) pollution from industry was
destroying the
ozone layer
in Earth's stratospher
in Earth's
stratosphere.
«Growing quantities of DCM are leaking into the
stratosphere, where it is exceptionally effective
in destroying the
ozone,» said David Rowley, an atmospheric chemist at the University College London, who was not involved
in the research.
Once water vapor gets into the normally dry
stratosphere, it can
in theory interact with manmade chlorine compounds known as chlorofluorocarbons, or CFC's, to
destroy ozone molecules.
Ozone in the
stratosphere is constantly being created and
destroyed by the action of light and photochemistry.
Secondly, human CFCs were
destroying ozone thus reducing its warming power
in the
stratosphere when the sun became more active.
An unusual persistence of cold temperatures
in the
stratosphere into March, allowing longer lifetimes for the polar stratospheric clouds that enable conversion of pollutant gases into
ozone -
destroying chlorine.
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.
The result would be a planet on which humans could work and survive outdoors
in the summer only
in mountainous regions [115,116]-- and there they would need to contend with the fact that a moist
stratosphere would have
destroyed the
ozone layer [117].
But this year, an Arctic counterpart emerged for the first time, thanks to unusually cold temperatures
in the
stratosphere plus lingering
ozone -
destroying pollutants.
It may be a matter of semantics, she concedes, but there was a rapid resupply of
ozone from outside the Arctic vortex (that swirling wall of winds
in the
stratosphere that largely corrals a patch of atmosphere, rendering it vulnerable to
ozone -
destroying chemical reactions).
Water vapor breaks down
in the
stratosphere, releasing reactive hydrogen oxide molecules that
destroy ozone.
It's now known that
ozone is
destroyed in the
stratosphere and that some human - released chemicals such as CFC's are speeding up the breakdown of
ozone, so that there are «holes» now
in our protective shield.