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The impact of anthropogenic chlorine emissions, stratospheric ozone change and chemical feedbacks on stratospheric water
anthropogenic chlorine emissions stratospheric ozone change chemical feedbacks
2009/2/25
Mixing ratios of water (H2O) in the stratosphere appear to increase due to increased input of H2O and methane from the troposphere and due to intensified oxidation of CH4 in the stratosphere, but many...
Radiative forcing since preindustrial times due to ozone change in the troposphere and the lower stratosphere
Radiative forcing preindustrial times ozone change troposphere lower stratosphere
2009/1/4
Changes in atmospheric ozone have occurred since the preindustrial era as a result of increasing anthropogenic emissions. Within ACCENT, a European Network of Excellence, ozone changes between 1850 a...