Poster's note : of interest to those evaluating ozone depletion from SRM ;
and cirrus stripping

http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate2451.html

A large ozone-circulation feedback and its implications for global warming
assessments

Peer J. Nowack, N. Luke Abraham, Amanda C. Maycock, Peter Braesicke,
Jonathan M. Gregory, Manoj M. Joshi, Annette Osprey & John A. Pyle

doi:10.1038/nclimate2451

Published online 01 December 2014

State-of-the-art climate models now include more climate processes
simulated at higher spatial resolution than ever1. Nevertheless, some
processes, such as atmospheric chemical feedbacks, are still
computationally expensive and are often ignored in climate simulations1, 2.
Here we present evidence that the representation of stratospheric ozone in
climate models can have a first-order impact on estimates of effective
climate sensitivity. Using a comprehensive atmosphere–ocean
chemistry–climate model, we find an increase in global mean surface warming
of around 1 °C (∼20%) after 75 years when ozone is prescribed at
pre-industrial levels compared with when it is allowed to evolve
self-consistently in response to an abrupt 4×CO2 forcing. The difference is
primarily attributed to changes in long-wave radiative feedbacks associated
with circulation-driven decreases in tropical lower stratospheric ozone and
related stratospheric water vapour and cirrus cloud changes. This has
important implications for global model intercomparison studies1, 2 in
which participating models often use simplified treatments of atmospheric
composition changes that are consistent with neither the specified
greenhouse gas forcing scenario nor the associated
atmospheric circulation feedbacks3, 4, 5.

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