Response of the stratospheric temperatures and ozone to past and future increases in stratospheric humidity
By V. Dvortsov, S. Solomon. 2001
155 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/c689e8e52a7d889355aed728a4befdb630a43417
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In Atmospheric Science
- William J. Randel
- Piers M. Forster
- Fei Wu
- D. Seidel
- S. Fueglistaler
- Karen H. Rosenlof
- D. Shindell
- Q. Fu
In Global and Planetary Change
Citations in the corpus
- Interannual changes of stratospheric water vapor and correlations with tropical tropopause temperatures (2004, background): “2000), and these positive trends can have significant radiative and chemical effects if representative of the global stratosphere (e.g., Forster and Shine 1999; Dvortsov and Solomon 2001; Shine et al. 2003).”
- Control of interannual and longer‐term variability of stratospheric water vapor (2005, background): “Introduction [2] Stratospheric water vapor plays an important role for the radiation budget of the troposphere [Held and Soden, 2000] as well as the stratosphere [Forster and Shine, 2002] and for stratospheric chemistry, in particular for ozone [Evans et al., 1998; Dvortsov and Solomon, 2001].”
- Multimodel projections of stratospheric ozone in the 21st century (2007, unknown): “[ 24 ] The recovery of ozone could also be affected by changes in stratospheric water vapor [ Kirk - Davidoff et al. , 1999; Dvortsov and Solomon , 2001; WMO / UNEP , 2007, chapter 5].”
- Assessing the climate impact of trends in stratospheric water vapor (2002, methodology): “05 ppmv/year increase in SWV modeled by Dvortsov and Solomon [2001] led to a very similar temperature response at 43 N.”
- Tropical tropopause layer (2009, background): “Stratospheric water vapor concentrations directly affect stratospheric HOx concentrations [e.g., Dvortsov and Solomon, 2001] and play a crucial role for the formation of polar stratospheric clouds that allow heterogeneous chemical reactions (involving chlorine species originating from…”
- A comparison of model‐simulated trends in stratospheric temperatures (2003, background): “The dominant reasons for these differences seem likely to be the particular radiation codes being used in models (Forster et al. (2001) – and see the spread in the Reading FDH results in Fig.”