The impact of anthropogenic chlorine emissions, stratospheric ozone change and chemical feedbacks on stratospheric water
Mixing ratios of water (H<sub>2</sub>O) in the stratosphere appear to increase due to increased input of H<sub>2</sub>O and methane from the troposphere and due to intensified oxidation of CH<sub>4</sub> in the stratosphere, but many of the underlying mechanisms a...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2004-01-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/4/693/2004/acp-4-693-2004.pdf |