https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020GL087929

Forcing Dependence of Atmospheric Lapse Rate Changes Dominates Residual
Polar Warming in Solar Radiation Management Climate Scenarios
Matthew Henry  Timothy M. Merlis
First published: 19 July 2020
https://doi.org/10.1029/2020GL087929
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Abstract
Simulations of solar radiation management (SRM) geoengineering using
comprehensive general circulation models show a residual surface warming at
high latitudes. Previous work attributes this to the difference in forcing
structure between the increase in greenhouse gases and decrease in
insolation, but this neglects the role of the induced reduction in
atmospheric energy transport. Here we show that the difference in vertical
structure of temperature change between increasing CO2, decreasing
insolation, and decreasing atmospheric energy transport is the dominant
reason for the residual near‐surface warming at high latitudes. A
single‐column model (SCM) is used to decompose the high‐latitude
temperature change and shows the importance of the enhanced near‐surface
warming from the CO2 increase in explaining the residual polar warming.
This suite of models invites caution when attributing high‐latitude surface
temperature changes to the lapse rate feedback, as various forcings and
nonlocal processes affect the vertical structure of temperature change
differently.

Plain Language Summary
Solar radiation management (SRM) geoengineering has been proposed as a way
of counteracting the warming effects of increasing greenhouse gases by
reflecting solar radiation. When the carbon dioxide concentration (CO2) is
quadrupled and the solar constant is reduced in climate models to reach
zero global mean surface temperature change, there is still residual
warming in polar regions. Previous analyses suggested that it was caused by
the latitudinal difference in forcing between the CO2 increase and
insolation reduction. This work shows the importance of the differences in
vertical structure of atmospheric temperature change between the CO2
increase and solar radiation reduction in explaining this residual polar
warming. This underlines the importance of considering the vertical
structure of temperature change caused by a given forcing when trying to
understand what shapes the pattern of surface temperature change.

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