Removal of chlorofluorocarbons by increased mass exchange between the stratosphere and troposphere in a changing climate
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Summary
It is predicted that, in response to the projected changes in greenhouse-gas concentrations during the first half of the twenty-first century, this rate of mass exchange will increase by 3% per decade, due to more vigorous extra-tropical planetary waves emanating from the troposphere.
- Type
- article
- Published
- 2001-04-12
- Cited by
- 298
- References
- 34
- OpenAlex
- https://openalex.org/W1503729094
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:4432154
Keywords
Stratosphere, Troposphere, Atmospheric sciences, Ozone layer, Environmental science
References
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- Stratospheric ozone transboundary transport to upper troposphere North Africa
- The evolution of the Brewer-Dobson circulation and the ozone layer during the last three decades
- Modelling the middle atmosphere and its sensitivity to climate change
- Climate dependencies and deterministic variability in stratospheric dynamics and ozone
- Caractérisation de la tropopause extratropicale avec les données aéroportées MOZAIC : zone de mélange et d'échange
- Contradictory Evidence on Wave Forcing of Tropical Upwelling in the Brewer-Dobson Circulation - A Suggested Resolution
- Attribution régionalisée des causes anthropiques du changement climatique
- Contributions to Future Stratospheric Climate Change: An Idealized Chemistry-Climate Model Sensitivity Study
- The Ozone Layer in the 21st Century
- Tracer-Independent Approaches to Stratosphere-Troposphere Exchange and Tropospheric Air Mass Composition
- The morphology of the Brewer–Dobson circulation and its response to climate change in CMIP5 simulations
- Sensitivity of 21st century stratospheric ozone to greenhouse gas scenarios
- Ozone and climate: A review of interconnections
- Unraveling impact factors for future changes in the Brewer‐Dobson circulation
- The Structure and Variability of the Tropical General Circulation
- UV sensitivity of planktonic net community production in ocean surface waters
- Long‐term changes in stratospheric age spectra in the 21st century in the Goddard Earth Observing System Chemistry‐Climate Model (GEOSCCM)
- Three dimensional chemical transport model study of ozone and related gases 1960-2000
- Long-term Climate Change: Projections, Commitments and Irreversibility
- Stratospheric Transport Changes Forced By Tropical Sea Surface Temperature Perturbation: Idealized Simulation
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