If I understand from the email below , you used aerosols with no fall
speed. Are experiments planned to simulate aerosol descent?

Andrew

On Mon, 16 Dec 2019, 05:43 Govindasamy Bala, <bala....@gmail.com> wrote:

> Andrews,
>
> We did not do experiments with aerosols above 22 km. It is likely that the
> cooling effect will be larger when aerosols are at 25 km. Beyond that it is
> likely that the additional cooling benefits disappear. We need more
> experiments to confirm this.
>
> The sensitivity to height in our paper arises mainly because of the
> increases in stratospheric water vapor (which partly offsets the cooling
> efficiency of the aerosols) that is associated with the stratospheric
> heating by the aerosols. This increase in stratospheric water vapor is
> largest when the aerosols (and the heating) is close to the tropopause.
>
> In our paper, we have isolated the effect of just one factor. As Doug has
> pointed out, the sedimentation effect would also lead to more cooling if
> aerosols are injected at higher altitudes...
>
> Best,
> Bala
>
> On Sun, Dec 15, 2019 at 9:05 PM Douglas MacMartin <dgm...@cornell.edu>
> wrote:
>
>> This is a great study to understand the effectiveness per unit mass **in
>> the stratosphere**.  Also keep in mind that there’s an additional
>> factor, that at lower altitudes it takes higher injection rates to achieve
>> the same burden in the stratosphere (i.e., lower lifetime at lower injected
>> altitude).
>>
>>
>>
>> If the only thing you cared about was cost, then since there are existing
>> studies demonstrating that you can design an aircraft to get to ~20-21km,
>> we roughly know that it could be done, but higher altitude injection means
>> less total sulfur injected and hence smaller side effects, and should be
>> better understood both on the modeling and implementation cost as the trade
>> may well be worth it.
>>
>>
>>
>> doug
>>
>>
>>
>> *From:* geoengineering@googlegroups.com <geoengineering@googlegroups.com>
>> *On Behalf Of *Govindasamy Bala
>> *Sent:* Saturday, December 14, 2019 9:38 PM
>> *To:* Andrew Lockley <andrew.lock...@gmail.com>
>> *Cc:* geoengineering <geoengineering@googlegroups.com>
>> *Subject:* Re: [geo] Climate system response to stratospheric sulfate
>> aerosols: sensitivity to altitude of aerosol layer
>>
>>
>>
>> Dear Andrew,
>>
>> Thanks for the posting. The heights studied were 16, 19 and 22 km, height
>> that are relevant to solar radiation modification problem.. The final
>> paragraph in the paper is worth reading to get more quantitative
>> information from this modeling study.
>>
>>
>>
>> "To summarize, for the same mass, the efficiency (defined
>>
>> as changes in surface temperature per Tg S) of volcanic
>> aerosol is less when it is prescribed at lower altitudes in the
>> stratosphere (Fig. 9). For example, in our simulations, there is
>> a surface cooling of 0.44K for each teragram of sulfur placed
>> in the stratosphere at about 16 km altitude (100 hPa). There
>> is an additional surface cooling of 0.15K per Tg S when the
>> prescribed altitude is increased from about 16 km to about
>> 22 km (37 hPa)."
>>
>>
>>
>> On Sat, Dec 14, 2019 at 12:55 AM Andrew Lockley <andrew.lock...@gmail.com>
>> wrote:
>>
>> Poster's note : this has significant implications for the engineering of
>> delivery systems. I can't do the pressure altitude conversion in my head,
>> but it's a lot higher than what's generally been planned for. We're gonna
>> need a bigger boat.
>>
>>
>>
>>
>>
>> https://www.earth-syst-dynam.net/10/885/2019/
>>
>>
>>
>> Climate system response to stratospheric sulfate aerosols: sensitivity to
>> altitude of aerosol layer
>>
>> *Krishna-Pillai Sukumara-Pillai Krishnamohan et al. *Received: 01 May
>> 2019 – Discussion started: 23 May 2019 – Revised: 24 Oct 2019 – Accepted:
>> 08 Nov 2019 – Published: 13 Dec 2019
>>
>> Abstract
>>
>> top <https://www.earth-syst-dynam.net/10/885/2019/#top>
>>
>> Reduction of surface temperatures of the planet by injecting sulfate
>> aerosols in the stratosphere has been suggested as an option to reduce the
>> amount of human-induced climate warming. Several previous studies have
>> shown that for a specified amount of injection, aerosols injected at a
>> higher altitude in the stratosphere would produce more cooling because
>> aerosol sedimentation would take longer. In this study, we isolate and
>> assess the sensitivity of stratospheric aerosol radiative forcing and the
>> resulting climate change to the altitude of the aerosol layer. We study
>> this by prescribing a specified amount of sulfate aerosols, of a size
>> typical of what is produced by volcanoes, distributed uniformly at
>> different levels in the stratosphere. We find that stratospheric sulfate
>> aerosols are more effective in cooling climate when they reside higher in
>> the stratosphere. We explain this sensitivity in terms of effective
>> radiative forcing: volcanic aerosols heat the stratospheric layers where
>> they reside, altering stratospheric water vapor content, tropospheric
>> stability, and clouds, and consequently the effective radiative forcing. We
>> show that the magnitude of the effective radiative forcing is larger when
>> aerosols are prescribed at higher altitudes and the differences in
>> radiative forcing due to fast adjustment processes can account for a
>> substantial part of the dependence of the amount of cooling on aerosol
>> altitude. These altitude effects would be additional to dependences on
>> aerosol microphysics, transport, and sedimentation, which are outside the
>> scope of this study. The cooling effectiveness of stratospheric sulfate
>> aerosols likely increases with the altitude of the aerosol layer both
>> because aerosols higher in the stratosphere have larger effective radiative
>> forcing and because they have higher stratospheric residence time; these
>> two effects are likely to be of comparable importance.
>>
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>> .
>>
>>
>>
>>
>> --
>>
>> With Best Wishes,
>>
>> -------------------------------------------------------------------
>> G. Bala
>> Professor
>> Center for Atmospheric and Oceanic Sciences
>> Indian Institute of Science
>> Bangalore - 560 012
>> India
>>
>> Tel: +91 80 2293 3428; +91 80 2293 2505
>> Fax: +91 80 2360 0865; +91 80 2293 3425
>> Email: gb...@iisc.ac.in; bala....@gmail.com
>> Web:http://dccc.iisc.ac.in/dr_govindasamy_bala_profile.html
>> -------------------------------------------------------------------
>>
>>
>>
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>> .
>>
>
>
> --
> With Best Wishes,
>
> -------------------------------------------------------------------
> G. Bala
> Professor
> Center for Atmospheric and Oceanic Sciences
> Indian Institute of Science
> Bangalore - 560 012
> India
>
> Tel: +91 80 2293 3428; +91 80 2293 2505
> Fax: +91 80 2360 0865; +91 80 2293 3425
> Email: gb...@iisc.ac.in; bala....@gmail.com
> Web:http://dccc.iisc.ac.in/dr_govindasamy_bala_profile.html
> -------------------------------------------------------------------
>
>

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