This paper comes to mind

https://www.science.org/doi/10.1126/sciadv.adk0593

Which proposes drying the stratosphere by seeding clouds at the tropopause

As I discussed in my previous email yesterday, Doug raised concerns about
H2 in Make Sunsets' balloons. I was also curious as to whether jet exhaust
might negate some / all of the climate benefit of SAI

https://www.youtube.com/live/_JBLMsXNmhs?si=57FK3DoOnV04edhN

On Mon, 18 Mar 2024, 23:01 Colin Forrest, <colinforre...@gmail.com> wrote:

> Researchers studying the aerosol burden after the Hunga Tonga Ha'apai
> eruption on the 15th of January 2022 found that the aerosols coagulated and
> fell out of the stratosphere faster than after the Pinotubo eruption. It is
> a submarine volcano in the Tongan archipelago in the southern  Pacific
> Ocean. The eruption at its height produced a series of four underwater
> thrusts, displaced 10 cubic kilometres (2.4 cu mi) of rock, ash and
> sediment, and generated the largest atmospheric explosion recorded by
> modern instrumentation.
>
> The researchers suggested that the faster rate of coagulation and
> sedimentation in the Hunga Tonga plume was due to the amount of seawater
> ejected.
>
> The consensus seems to be that fixed-wing jet aircraft are the way forward
> (or up) for SAI, so we need to take into acount the number of flights
> crossing the tropopause, which increases mixing across the tropopause, and
> the amount of CO2 and H2O added and O2 removed from the stratosphere in
> bulk terms, due to the combustion of jet fuel..
>
> As the aircraft exhaust and the aerosol will be mixed into the plume
> together at high temperature in the early moments when coagulation can
> happen rapidly, the amount of water added to the plume may have a
> significant effect on coagulation and sedimentation rates. Therefore
> accurately modelling the amount of fuel burnt while deploying the aerosol
> could be important, as at may affect the atmospheric lifetime of the
> injected aerosol.
>
> Best Regards,  Colin Forrest
>
>
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