https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019GL083701

Climate Response to Pulse Versus Sustained Stratospheric Aerosol Forcing
Lei Duan
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorStored=Duan%2C+Lei>


Long Cao
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorStored=Cao%2C+Long>


Govindasamy Bala
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorStored=Bala%2C+Govindasamy>


Ken Caldeira
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorStored=Caldeira%2C+Ken>
First published: 05 August 2019
https://doi.org/10.1029/2019GL083701
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Abstract

Solar geoengineering has been suggested as a potential means to counteract
anthropogenic warming. Major volcanic eruptions have been used as natural
analogues to large‐scale deployments of stratospheric aerosol
geoengineering, yet difference in climate responses to these forcings
remains unclear. Using the National Center for Atmospheric Research
Community Earth System Model, we compare climate responses to two highly
idealized stratospheric aerosol forcings that have different durations: a
short‐term pulse representative of volcanic eruptions and a long‐term
sustained forcing representative of geoengineering. For the same amount of
global mean cooling, decreases in land temperature, precipitation, and
runoff in the pulse case are much larger than that in the sustained case.
The spatial pattern changes differ substantially between these two cases.
Thus, direct extrapolations from volcanic eruption observations provide
limited insight into impacts of potential stratospheric aerosol
geoengineering. However, simulations of volcanic eruptions can be useful to
test process representations in models that are used to simulate
geoengineering deployments

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