30 hPa is about 25kms. That's pretty normal for release studies. See for
example Aurora flight services report

I'm doing a paper at present which shows you can loft a shell that high for
very little money - probably an order of magnitude cheaper than Aurora
calculated. I've not finished the calcs yet.

You could hit those costs using an extended Mark 7 Iowa class 16 in gun.
Methane/air propellant should get you to 25k, but using a H2 / O2
propellant (run rich) can get far higher by improving speed of sound.  To
cut shell mass you can use an enlarged, fin-stabilized aluminum or titanium
shell. Projectiles would splashdown, to be reused or scrapped.

A
 On Jun 29, 2012 4:33 PM, "Simone Tilmes" <[email protected]> wrote:

> Dear Ken,
>
> thanks a lot to Matthias, to translate the article!
>
> I think it is important to point out that there is very likely a limit on
> how much the Earth's surface could be cooled using sulfate aerosols, due to
> coagulation processes and fall out of aerosols. Only less than 2 W/m2
> reduction of global net surface SW flux was achieved in the study by
> Heckendorn et al., 2009, using a micro-physical model to consider size
> distributions of the aerosols. Niemeier et al., 2010, achieved a stronger
> forcing if injecting particles at 30hPa, which allow them to stay longer in
> the stratosphere. Though it will be hard to inject particles that high.
>
> Cheers, Simone
>
> References:
> Niemeier, U., H. Schmidt and C. Timmreck, The dependency of geoengineered
> sulfate aerosol on the emission strategy, Atmos. Sci. Let., DOI:
> 10.1002/asl.304, 2010.
>
> Heckendorn P, Weisenstein D, Fueglistaler S, Luo BP, Rozanov E, Schraner
> M, Thomason LW, Peter T. 2009. The impact of geoengineering aerosols on
> stratospheric temperature and ozone.
> Environmental Research Letters 4: 045108. DOI:
> 10.1088/1748-9326/4/4/045108.
>
>
>
>  Simone,
>>
>> Not reading German, I don't know precisely what is in the story.
>>
>> What I said to the reporter is that if the aerosol layer similar to that
>> of Mt Pinatubo were sustained, it would produce a cooling of about 3 K.
>>
>> This is based on estimates of Mt Pinatubo producing around 4 W / m2 of
>> radiative forcing (cf. Crutzen, 2006?), which is similar to a CO2
>> doubling -- and 3 C per CO2 doubling is in the middle of the range of
>> estimates for climate sensitivity. So, this is just a back-of-envelope
>> calculation.
>>
>> A question of course, given particle aggregation and so on, is whether
>> such a layer could be sustained.
>>
>> Best,
>>
>> Ken
>>
>>
>> On Thu, Jun 28, 2012 at 6:37 PM, Simone Tilmes <[email protected]
>> <mailto:[email protected]>> wrote:
>>
>>    Dear Ken,
>>
>>    in the article you stated that Mt Pinatubo is assumed to result in a
>>    global cooling of about 0.5 degree. It is also stated in the text of
>>    the article that the amount of aerosols emitted, if they would stay
>>    in the stratosphere for a longer time period, would result in a 3
>>    degrees global cooling. Could you point me to the study you are
>>    referring to that calculates this amount of cooling if injecting
>>    volcanic aerosols of the amount of Mt Pinatubo?
>>
>>    Cheers, Simone
>>
>>
>>        Ken
>>
>>        It should follow from your argument about the land-sea temperature
>>        difference reducing precipitation on land that a technique which
>>        had the
>>        initial effect of cooling the sea would be more attractive.  If
>>        it were
>>        also possible to have a frequency response shorter than the monsoon
>>        cycle we could play useful tricks about the phase of operations
>>        relative
>>        to the monsoon season.
>>
>>        Stephen
>>
>>        Emeritus Professor of Engineering Design
>>        Institute for Energy Systems
>>        School of Engineering
>>        Mayfield Road
>>        University of Edinburgh EH9  3JL
>>        Scotland
>>        Tel +44 131 650 5704 <tel:%2B44%20131%20650%205704>
>>        Mobile 07795 203 195
>>        www.see.ed.ac.uk/~shs <http://www.see.ed.ac.uk/~shs>
>>
>>
>>        On 28/06/2012 06:27, Ken Caldeira wrote:
>>
>>            pdf attached.
>>
>>            http://www.nzz.ch/wissen/__**wissenschaft/sonnenschutz-__**
>> fuer-die-erde-1.17282213<http://www.nzz.ch/wissen/__wissenschaft/sonnenschutz-__fuer-die-erde-1.17282213>
>>            <http://www.nzz.ch/wissen/**wissenschaft/sonnenschutz-**
>> fuer-die-erde-1.17282213<http://www.nzz.ch/wissen/wissenschaft/sonnenschutz-fuer-die-erde-1.17282213>
>> >
>>
>>
>>            _______________
>>            Ken Caldeira
>>
>>            Carnegie Institution for Science
>>
>>            Dept of Global Ecology
>>            260 Panama Street, Stanford, CA 94305 USA
>>            +1 650 704 7212 <tel:%2B1%20650%20704%207212>
>>            [email protected]
>>            
>> <mailto:kcaldeira@**carnegiescience.edu<[email protected]>
>> >
>>            
>> <mailto:kcaldeira@__carnegiesc**ience.edu<http://carnegiescience.edu>
>>            
>> <mailto:kcaldeira@**carnegiescience.edu<[email protected]>
>> >>
>>            
>> http://dge.stanford.edu/labs/_**_caldeiralab<http://dge.stanford.edu/labs/__caldeiralab>
>>            
>> <http://dge.stanford.edu/labs/**caldeiralab<http://dge.stanford.edu/labs/caldeiralab>>
>> @kencaldeira
>>
>>            *Currently visiting * Institute for Advanced Sustainability
>>            Studies
>>            (IASS) <http://www.iass-potsdam.de/>
>>            *and *Potsdam Institute for Climate Impact Research (PIK)
>>            <http://www.pik-potsdam.de/>*_**_in Potsdam, Germany.*
>>
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