The Chemical Sensitivity of Stratospheric Ozone to N₂O and CH₄ through the 21st century
Through the 21st century, global-mean stratospheric ozone abundances are projected to increase due to decreasing chlorine and bromine concentrations (as a consequence of the Montreal Protocol for Substances that Deplete the Ozone Layer), and continued CO₂-induced cooling of the stratosphere. Along w...
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| Language: | en |
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University of Canterbury. Chemistry
2012
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| Online Access: | http://hdl.handle.net/10092/7170 |