https://iopscience.iop.org/article/10.1088/1748-9326/ab71a3

To what extent can cirrus cloud seeding counteract global warming?
Blaž Gasparini1, Zachary McGraw2, Trude Storelvmo2 and Ulrike Lohmann3

Accepted Manuscript online 30 January 2020 • © 2020 The Author(s).
Published by IOP Publishing Ltd
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Abstract
The idea of modifying cirrus clouds to directly counteract greenhouse gas
warming has gained momentum in recent years, despite disputes over its
physical feasibility. Previous studies that analyzed modifications of
cirrus clouds by seeding of ice nucleating particles showed large
uncertainties in both cloud and surface climate responses, ranging from no
effect or even a small warming to a globally averaged cooling of about
2.5°C. We use two general circulation models that showed very different
responses in previous studies, ECHAM6-HAM and CESM-CAM5, to determine which
radiative and climatic responses to cirrus cloud seeding in a 1.5 x CO2
world are common and which are not. Seeding reduces the net cirrus
radiative effect for -1.8 W m-2 in CESM compared with only -0.8 W m-2 in
ECHAM. Accordingly, the surface temperature decrease is larger in CESM,
counteracting about 70% of the global mean temperature increase due to CO2
and only 30% in ECHAM. While seeding impacts on mean precipitation were
addressed in past studies, we are the first to analyze extreme
precipitation responses to cirrus seeding. Seeding decreases the frequency
of the most extreme precipitation globally. However, the extreme
precipitation events occur more frequently in the Sahel and Central
America, following the mean precipitation increase due to a northward shift
of the Intertropical Convergence Zone. In addition, we use a quadratic
climate damage metric to evaluate the amount of CO2 -induced damage cirrus
seeding can counteract. Seeding decreases the damage by about 50% in ECHAM,
and by 85% in CESM over the 21 selected land regions. Climate damage due to
CO2 increase is significantly reduced as a result of seeding in all of the
considered land regions.

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