And the final version of the paper just came out yesterday

https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2020GL089470?af=R 
<https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2020GL089470?af=R>

if anyone’s interested!

Dan
















> On 4 Sep 2020, at 07:41, Andrew Lockley <andrew.lock...@gmail.com> wrote:
> 
> Interview with Dan about this paper on the Reviewer 2 podcast 
> https://open.spotify.com/episode/0Ic5LLIcL0UvhBnXDQT3HE?si=nbRuQuiUSceDtaQeb11z4w
>  
> <https://open.spotify.com/episode/0Ic5LLIcL0UvhBnXDQT3HE?si=nbRuQuiUSceDtaQeb11z4w>
> On Sat, 11 Jul 2020, 08:40 Andrew Lockley, <andrew.lock...@gmail.com 
> <mailto:andrew.lock...@gmail.com>> wrote:
> https://www.essoar.org/doi/abs/10.1002/essoar.10503509.1 
> <https://www.essoar.org/doi/abs/10.1002/essoar.10503509.1>
> 
> Reduced poleward transport due to stratospheric heating under geoengineering
> Authors
> Daniele Visioni
> iD
> Isla Ruth Simpson
> iD
> Douglas G MacMartin
> iD
> Jadwiga H. Richter
> Ben Kravitz
> iD
> Walker Lee
> See all authors 
> Published Online:Sun, 5 Jul 2020
> DOI:https://doi.org/10.1002/essoar.10503509.1 
> <https://doi.org/10.1002/essoar.10503509.1>
> Download PDF
> About
> Tools
>  
> Abstract
> By injecting SO2 into the stratosphere at different latitudes, it might be 
> possible to reduce global mean surface temperature and to minimize changes in 
> the equator-to-pole and inter-hemispheric gradients, reducing some of the 
> impacts arising from climate change relative to equatorial SO2 injection. 
> This can happen only if the resulting aerosols are transported to higher 
> latitudes by the stratospheric circulation, ensuring that a greater part of 
> the solar radiation is reflected back to space at higher latitudes, 
> compensating for the reduced sunlight there. However, the stratospheric 
> heating produced by these aerosols modifies the global circulation and 
> strengthens the stratospheric polar vortex that acts as a barrier to the 
> transport of air towards the poles. We show how this heating results in a 
> nonlinear feedback where increasing injection rates lead to a stronger high 
> latitudinal transport barrier. This implies a potential limitation in the 
> high-latitude aerosol burden and subsequent high-latitude cooling.

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