As discussed in my original post, a significant scaling of synthetic cosmic
rays is possible, over background levels (3-5 orders) This may give a large
climate signal, sufficient to analyse the effect with a view to using it
for CE.

Does anyone have a view on the potential usefulness of high-volume,
standard-energy cosmic rays?

A

On Sun, 19 Aug 2018, 16:35 Olivier Boucher, <[email protected]>
wrote:

>
> Hello Andrew,
>
> see section 7.4.6 of IPCC AR5 :
> http://www.ipcc.ch/pdf/assessment-report/ar5/wg1/WG1AR5_Chapter07_FINAL.pdf
>
> The summary is
>
> "Cosmic rays enhance new particle formation in the free troposphere, but
> the effect on the concentration of cloud condensation nuclei is too weak to
> have any detectable climatic influence during a solar cycle or over the
> last century (medium evidence, high agreement). No robust association
> between changes in cosmic rays and cloudiness has been identified. In the
> event that such an association existed, a mechanism other than cosmic
> ray-induced nucleation of new aerosol particles would be needed to explain
> it. {7.4.6}"
>
> Best
>
> Olivier
>
> Cosmic rays cause cloud condensation nuclei. They are therefore believed
> to affect cloudiness, and therefore climate. If we made more cosmic rays,
> that would likely make it more cloudy. Whether this was a warming or
> cooling effect would depend on whether it was cirrus or cumulus clouds (NB,
> sometimes making cirrus ultimately removes water, resulting in less
> cirrus)
>
> Cosmic rays are almost all protons, with an typical energy peak
> distribution of 0.3GEv. (4.8×10−11 J). No idea if that's the right energy
> for CCN, but we can tweak that later.
>
> Creating artificial cosmic rays is possible, using a linear particle
> accelerator. This is similar to an ion thruster, as used in space probes.
>
> To affect climate, you'd probably have to get densities of the order of
> 1/s/sqm (more on that, later).
>
> 360 million square kilometers of ocean is 360tn sqm or 3.6x10^14sqm. You
> don't really want to send particles into people, and the cleaner air over
> the oceans makes them more effective.
>
> A kilo of hydrogen contains 6x10^26 protons.
>
> That means 1kg of H2 gives you enough material for 1.6x10^12s = roughly 50
> years - so a satellite could easily carry enough material to do the job.
>
> Power is 3.6x10^14 x 4.8x10^-11J/s = 17kW - again, well within what a
> satellite could muster (roughly 100sqm of solar panels, at around 20% panel
> efficiency (conservative) and 50pc conversion (made up) efficiency).
>
> Cheap satellites are about $50m - well within the capabilities of a rich
> philanthropist. Even if this is not cheap, it's still only perhaps 500m
>
> If I'm out by 5 orders (1 ray per sq cm, not per sq m each second), then
> that's only 10,000 satellites. That's expensive, but not outlandish.
> Superficially, that would be $500bn at the lower cost, but there is likely
> a 10x or 100x experience curve cost reduction, meaning the whole programme
> would be about $5-50bn max.
>
> As an alternative, you could use aircraft or balloons, but beam
> attenuation would be a serious issue. 40km balloons can be launched, albeit
> with small payloads. They would fly at the bottom of the mesosphere, over
> 99.9pc of the atmosphere. So maybe beam attenuation would be tolerable, at
> that height. I don't know how to calculate it, but I'm guessing it would be
> cms to kms - so not really far enough to make a difference to climate. You
> could perhaps have mountaintop accelerators with very high powers, and a
> sweeping beam (like a lighthouse). If the power requirement was GW-range,
> then maybe the beam range would be a hundred km, or so. That might be
> enough to work, but it would have some pretty significant effects on local
> atmospheric chemistry - so probably not a good idea.
>
> Any thoughts from anyone?
>
> Andrew Lockley
>
>
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> --
> ------------------------------
> BAMS State of the Climate 2017
> <https://www.ametsoc.org/ams/index.cfm/publications/bulletin-of-the-american-meteorological-society-bams/state-of-the-climate/>
> has an aerosol section in the Global Climate chapter
>
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