https://esd.copernicus.org/articles/13/1233/2022/

Indices of extremes: geographic patterns of change in extremes and
associated vegetation impacts under climate intervention
Mari R. Tye et al.
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Received: 10 Feb 2022 – Discussion started: 14 Mar 2022 – Revised: 14 Jul
2022 – Accepted: 08 Aug 2022 – Published: 26 Aug 2022
Abstract
Extreme weather events have been demonstrated to be increasing in frequency
and intensity across the globe and are anticipated to increase further with
projected changes in climate. Solar climate intervention strategies,
specifically stratospheric aerosol injection (SAI), have the potential to
minimize some of the impacts of a changing climate while more robust
reductions in greenhouse gas emissions take effect. However, to date little
attention has been paid to the possible responses of extreme weather and
climate events under climate intervention scenarios. We present an analysis
of 16 extreme surface temperature and precipitation indices, as well as
associated vegetation responses, applied to the Geoengineering Large
Ensemble (GLENS). GLENS is an ensemble of simulations performed with the
Community Earth System Model (CESM1) wherein SAI is simulated to offset the
warming produced by a high-emission scenario throughout the 21st century,
maintaining surface temperatures at 2020 levels.

GLENS is generally successful at maintaining global mean temperature near
2020 levels; however, it does not completely offset some of the projected
warming in northern latitudes. Some regions are also projected to cool
substantially in comparison to the present day, with the greatest decreases
in daytime temperatures. The differential warming–cooling also translates
to fewer very hot days but more very hot nights during the summer and fewer
very cold days or nights compared to the current day. Extreme precipitation
patterns, for the most part, are projected to reduce in intensity in areas
that are wet in the current climate and increase in intensity in dry areas.
We also find that the distribution of daily precipitation becomes more
consistent with more days with light rain and fewer very intense events
than currently occur. In many regions there is a reduction in the
persistence of long dry and wet spells compared to present day. However,
asymmetry in the night and day temperatures, together with changes in cloud
cover and vegetative responses, could exacerbate drying in regions that are
already sensitive to drought. Overall, our results suggest that while SAI
may ameliorate some of the extreme weather hazards produced by global
warming, it would also present some significant differences in the
distribution of climate extremes compared to the present day.

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