Climate and ozone response to increased stratospheric water vapor

By D. Shindell. 2001

189 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5428e5ff57b4a83cbd15620b384edbec6ed7ee9d

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Citations in the corpus

Reconstruction of solar total irradiance since 1700 from the surface magnetic flux (2007, background): “…directly measured, are possibly of even greater importance for the global climate change (e.g., Eddy 1976; Reid 1987; Bond et al. 2001; Haigh 2001; Shindell 2001; Rind 2002; Stott et al. 2003), since the coupled system of the Earth’s atmosphere and oceans reacts rather slowly to the varying solar…”
Non-CO2 greenhouse gases and climate change (2011, background): “For example, increased atmospheric CH 4 enhances stratospheric water vapour and tropospheric ozone, and also affects aerosol”
Multimodel projections of stratospheric ozone in the 21st century (2007, unknown): “A strengthening of the Brewer-Dobson circulation might also increase polar downwelling, which would counteract the GHG-induced cooling of the polar stratosphere [ Manzini et al. , 2003].”
Observations of deep convective influence on stratospheric water vapor and its isotopic composition (2007, background): “Reliable longterm climate forecasts therefore require accurate descriptions of the response of stratospheric H2O to changes in climate forcing [Shindell, 2001; Forster and Shine, 2002].”
Assessing the climate impact of trends in stratospheric water vapor (2002, methodology): “7 ppmv), noting that Smith et al. [2001], using more refined trends and background climatology, derived a forcing consistent with our initial estimate of 0.19 Wm (2). [8] The degree of approximation employed for our applied perturbation in FS99 was felt justified by the paucity of longterm SWV measu”
State of the climate in 2010 (2011, background): “S70 | JUNE 2011 Stratospheric water vapor modulates Earth’s climate, directly through long-wave radiative processes, and indirectly through its influence on stratospheric ozone abundance (Shindell 2001).”
Modeling atmospheric stable water isotopes and the potential for constraining cloud processes and stratosphere‐troposphere water exchange (2005, background): “: MODELING ATMOSPHERIC STABLE WATER ISOTOPES 3 of 15 D21314 variability is crucial to assessing the causes of recent climate changes [Forster and Shine, 1999; Shindell, 2001].”
Climate forcings in Goddard Institute for Space Studies SI2000 simulations (2002, background): “The ozone change associated with the solar cycle almost certainly provides a positive amplification of the direct solar forcing, but it is complex and may depend significantly on the background state of the stratosphere [Shindell et al., 2001].Haigh [1994] points out that increased ultraviolet radia”