Stratospheric temperature trends: Observations and model simulations
By V. Ramaswamy, M. Chanin, J. Angell, J. Barnett, D. Gaffen, M. Gelman, P. Keckhut, Y. Koshelkov, K. Labitzke, Jj J. Lin and 7 more. 2001
399 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d1d0024b9cff7966506b2f5f3fe472e5d0bbb6db
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In Atmospheric Science
- William J. Randel
- Piers M. Forster
- D. Seidel
- T. G. Shepherd
- D. Shindell
- Stephen A. Klein
- Fei Wu
- J. Haigh
In Global and Planetary Change
- William J. Randel
- Piers M. Forster
- D. Shindell
- D. Seidel
- T. G. Shepherd
- Stephen A. Klein
- Fei Wu
- Gerald A. Meehl
Citations in the corpus
- A comparison of model‐simulated trends in stratospheric temperatures (2003, methodology): “…lack of any other temperature trend data to provide corroborative evidence for the SSU trends in the middle and upper stratosphere at the global scale is unfortunate; Ramaswamy et al. (2001) note that a variety of corrections have to be made to the SSU data that may impact on the derived trends.”
- An update of observed stratospheric temperature trends (2009, positive): “[29] Estimates of trends are derived using a multivariate linear regression analysis, as in the paper by Ramaswamy et al. [2001]. The statistical model includes terms to account for linear trends, together with variability associated with the 11-year solar cycle (using the solar F10.”
- Stratospheric microbiology at 20 km over the Pacific Ocean (2010, background): “First, the very low temperature of the sampling environment (-75C) in this study was far below -20C, the minimum temperature for microbial growth reported to date ( Price and Sowers 2004; Junge et al. 2006).”
- Climate forcings in Goddard Institute for Space Studies SI2000 simulations (2002, methodology): “[144] Climate forcings have a strong effect on the atmospheric temperature profile, as illustrated explicitly in Figure 6 of F-C and by Ramaswamy et al. [2001]. We do not attempt a comprehensive study here, which would require more real-”
- Dynamics, stratospheric ozone, and climate change (2008, background): “Increased CO2 is expected to cool the stratosphere, with the cooling being greatest for the highest temperatures and thus in the upper stratosphere, and such cooling is well documented in observations (Ramaswamy et al., 2001; see also Fig.”
- Behavior of tropopause height and atmospheric temperature in models, reanalyses, and observations: Decadal changes (2003, methodology): “A useful review is given by Ramaswamy et al. [2001].”