A comparison of model‐simulated trends in stratospheric temperatures

By K. Shine, M. Bourqui, Piers M. Forster, Sylvia H. E. Hare, U. Langematz, P. Braesicke, V. Grewe, M. Ponater, C. Schnadt, Claire A. Smith and 13 more. 2003

225 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/d062db5479a9bfbbc9b84d58417c276dff3103d3

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Citations in the corpus

Response of the large‐scale structure of the atmosphere to global warming (2015, background): “Stratospheric cooling as a response to increased GHGs has been found in models going back at least to Manabe and Wetherald (1967) and Shine et al. (2003) note that there is strong evidence that the stratosphere has in fact cooled over recent decades.”
An update of observed stratospheric temperature trends (2009, unknown): “…source of data on temperature trends above the lower stratosphere over such a long period; it has been extensively used in assessments of those trends, and their possible causes [e.g., Nash and Forrester , 1986; Ramaswamy et al. , 2001; Shine et al. , 2003; WMO , 2006; Cagnazzo et al. , 2006].”
Interannual changes of stratospheric water vapor and correlations with tropical tropopause temperatures (2004, background): “…(40ЊN), have shown positive trends of ϳ1% yr Ϫ1 for the period 1980– 2000 (Oltmans et al. 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).”
An assessment of three alternatives to linear trends for characterizing global atmospheric temperature changes (2004, unknown): “Stratospheric ozone loss and increases in well-mixed greenhouse gases [Ramaswamy et al., 2001; Hansen et al., 2002; Hare et al., 2004; Shine et al., 2003], or gradually increasing stratospheric water vapor [Forster and Shine, 2002], have been suggested as causes of the observed cooling.”
Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection (2008, background): “[20] The standard World Meteorological Organisation (WMO) definition of the tropopause, i.e., the lowest point at which the lapse rate drops below 2 Ck m 1 and remains there for at least 2 km, can be applied in the tropics as well as in midlatitudes, but tropical radiosonde profiles often reveal the”
A stratospheric ozone profile data set for 1979–2005: Variability, trends, and comparisons with column ozone data (2007, background): “Modeling studies also confirm that ozone loss is a dominant mechanism leading to cooling of the lower stratosphere since 1980 [Langematz et al., 2003; Shine et al., 2003; Dameris et al., 2005; Ramaswamy et al., 2006].”
CMIP5 historical simulations (1850–2012) with GISS ModelE2 (2014, background): “The exceptional cooling over Antarctica represents the combined effect of increasing greenhouse gas concentrations and stratospheric ozone depletion [Shine et al., 2003].”