Is the climate sensitivity to ozone perturbations enhanced by stratospheric water vapor feedback?
- 1 August 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (15) , 2887-2890
- https://doi.org/10.1029/2001gl013000
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Stratosphere adjusted radiative forcing calculationsin a comprehensive climate modelTheoretical and Applied Climatology, 2001
- Stratospheric water vapour changes as a possible contributor to observed stratospheric coolingGeophysical Research Letters, 1999
- Radiative forcing and climate sensitivity: The ozone experienceQuarterly Journal of the Royal Meteorological Society, 1999
- Transient Climate Change Simulations with a Coupled Atmosphere–Ocean GCM Including the Tropospheric Sulfur CycleJournal of Climate, 1999
- Tropospheric Water Vapor and Climate SensitivityJournal of the Atmospheric Sciences, 1999
- Why is the global warming proceeding much slower than expected?Journal of Geophysical Research: Atmospheres, 1999
- A reexamination of the “stratospheric fountain” hypothesisGeophysical Research Letters, 1998
- Simulation of the Meridionally and Seasonally Varying Climate Response Caused by Changes in Ozone ConcentrationJournal of Climate, 1997
- Radiative forcing and climate responseJournal of Geophysical Research: Atmospheres, 1997
- Modeled impacts of stratospheric ozone and water vapor perturbations with implications for high‐speed civil transport aircraftJournal of Geophysical Research: Atmospheres, 1995