http://www.agu.org/pubs/crossref/pip/2012JD017607.shtml

The ability of the climate models submitted to the Coupled Model
Intercomparison Project 5 (CMIP5) database to simulate the Northern
Hemisphere winter climate following a large tropical volcanic eruption is
assessed. When sulfate aerosols are produced by volcanic injections into
the tropical stratosphere and spread by the stratospheric circulation, it
not only causes globally averaged tropospheric cooling but also a localized
heating in the lower stratosphere, which can cause major dynamical
feedbacks. Observations show a lower stratospheric and surface response
during the following one or two Northern Hemisphere (NH) winters, that
resembles the positive phase of the North Atlantic Oscillation (NAO).
Simulations from 13 CMIP5 models that represent tropical eruptions in the
19th and 20th century are examined, focusing on the large-scale regional
impacts associated with the large-scale circulation during the NH winter
season. The models generally fail to capture the NH dynamical response
following eruptions. They do not sufficiently simulate the observed
post-volcanic strengthened NH polar vortex, positive NAO, or NH Eurasian
warming pattern, and they tend to overestimate the cooling in the tropical
troposphere. The findings are confirmed by a superposed epoch analysis of
the NAO index for each model. The study confirms previous similar
evaluations and raises concern for the ability of current climate models to
simulate the response of a major mode of global circulation variability to
external forcings. This is also of concern for the accuracy of
geoengineering modeling studies that assess the atmospheric response to
stratosphere-injected particles.Received 13 February 2012; accepted 24 July
2012.

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