Dynamics, stratospheric ozone, and climate change

By T. G. Shepherd. 2008

175 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a5b67510199fa2b982364ef2c440b6f36065d830

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Citations in the corpus

A Robust Mechanism for Strengthening of the Brewer–Dobson Circulation in Response to Climate Change: Critical-Layer Control of Subtropical Wave Breaking (2011, methodology): “Furthermore, the good agreement between CMAM and observations (Eyring et al. 2006; Waugh and Eyring 2008; Shepherd 2008; MS09) gives credence to the future changes.”
Large climate-induced changes in ultraviolet index and stratosphere-to-troposphere ozone flux (2009, background): “, interest has turned to the effects of climate change on the ozone laye”
Assessing and understanding the impact of stratospheric dynamics and variability on the earth system (2012, background): “If the Brewer–Dobson circulation does increase, leading to greater mass transport from the tropics to the extratropics, then tropical ozone may never recover to preindustrial levels, while extratropical ozone will become larger than ever before (Shepherd 2008; Waugh et al. 2009a).”
THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, background): “This increased Brewer‐ Dobson circulation implies an increase in ozone in the extratropical LMS [Shepherd, 2008; Li et al., 2009; Gettelman et al., 2010] and in the mass of STE [Sudo et al.”
High‐latitude influence of the quasi‐biennial oscillation (2014, background): “…time wrapping diagonally about the cylinder.) time-scales is relevant to issues such as ozone depletion and recovery (e.g. Austin et al., 2003; Shepherd, 2008), stratosphere–troposphere coupling including the possible downward influence of the stratosphere on the troposphere (e.g. Baldwin and…”
Observed temporal evolution of global mean age of stratospheric air for the 2002 to 2010 period (2011, background): “…increasing levels of greenhouse gases is a possible change in the stratospheric circulation (Butchart et al., 2006) with substantial feed-backs on chlorofluorocarbon lifetimes (Butchart and Scaife, 2001; Douglass et al., 2008), ozone (Shepherd, 2008) and the climate system (Baldwin et al., 2007).”