Here's a new paper of ours. Keep in mind that it analyses an
extreme scenario, from GLENS at the end of the century.
Banerjee, Antara, Amy H. Butler, Lorenzo M. Polvani, Alan Robock,
Isla R. Simpson, and Lantao Sun, 2021: Robust winter warming over
Eurasia under stratospheric sulfate geoengineering – the role of
stratospheric dynamics.
Atm. Chem. Phys.,
21,
6985-6997, doi:10.5194/acp-21-6985-2021.
https://acp.copernicus.org/articles/21/6985/2021/
Abstract
It has been suggested that increased stratospheric sulfate aerosol
loadings following large, low latitude volcanic eruptions can lead
to wintertime warming over Eurasia through dynamical
stratosphere–troposphere coupling. We here investigate the proposed
connection in the context of hypothetical future stratospheric
sulfate geoengineering in the Geoengineering Large Ensemble
simulations. In those geoengineering simulations, we find that
stratospheric circulation anomalies that resemble the positive phase
of the Northern Annular Mode in winter are a distinguishing climate
response which is absent when increasing greenhouse gases alone are
prescribed. This stratospheric dynamical response projects onto the
positive phase of the North Atlantic Oscillation, leading to
associated side effects of this climate intervention strategy, such
as continental Eurasian warming and precipitation changes.
Seasonality is a key signature of the dynamically driven surface
response. We find an opposite response of the North Atlantic
Oscillation in summer, when no dynamical role of the stratosphere is
expected. The robustness of the wintertime forced response stands in
contrast to previously proposed volcanic responses.