I agree with Stephen, a hypothetical fleet of spray vessels would be
relatively secure.  In practice, such a fleet would constitute a
global CCN navy that would likely never be deployed without the
consent of the great powers, including the few major naval powers (US,
Russia, UK, ~China).  These ships would be numerous, dispersed, and
protected by the international community.  No private group or
corporation would possess the resources necessary to significantly
disrupt their operations - indeed, the only governments with such a
capability would have to sign off on the idea in the first place.

Beyond this, as Kelly notes, sulfur and CCN is not an either/
proposition - they may well serve as complementary intervention
strategies.

Josh Horton


On Feb 12, 5:50 am, Stephen Salter <[email protected]> wrote:
> Andrew
>
> I think that you may be mistaken about the vulnerability of spray
> vessels. They will be widely dispersed in remote parts of the ocean.  It
> will be slow and expensive to knock out large numbers of them. Their
> loss will take some time to hurt.  Attacking ships will be visible on
> radar for a day or so before they get close.  Attacking aircraft can be
> intercepted on their return flight. Either will be much more expensive
> that a spray vessel.  If I wanted to destroy  human existence I could
> think of much more damaging ways to do it.
>
> During WWII the Americans were building three 14,000 ton Liberty ships a
> day which was faster than the U boats could sink them. Mean construction
> time was seven weeks but one was built in less than 5 days.  Spray
> vessels will be only 300  tons each and we can get the Chinese to help.
>
> Stephen
>
> Emeritus Professor of Engineering Design
> School of Engineering and Electronics
> University of Edinburgh
> Mayfield Road
> Edinburgh EH9 3JL
> Scotland
> tel +44 131 650 5704
> fax +44 131 650 5702
> Mobile  07795 203 195
> [email protected]http://www.see.ed.ac.uk/~shs   
>
>
>
>
>
> Andrew Lockley wrote:
> > There's another fairly critical issue about cloud ships that's rarely
> > considered, and that's their vulnerability.  Let's image we're 50
> > years into a geoengineering programme, with either CCN or sulfur, and
> > let's say we've got an 8C warming effect.  In the sulfur world, we'll
> > be using a firehose, tanker fleet, or gunnery to shift the sulfur.
> >  You won't be able to get near any of that infrastructure if you fancy
> > throwing a spanner in the works.
>
> > Not so the cloud ships.  They will be floating about autonomously in
> > the sea, and if anyone doesn't like them, they're quite free to set
> > fire to them, blow them up, or just hack their software.  Trying to
> > build them all again in a hurry when we're already in the midst of 8C
> > warming could be a serious problem.  They won't be terribly expensive,
> > but would a few months/years of 8C be highly damaging, or would the
> > heat capacity of the ocean save our bacon?
>
> > It's a point that needs to be clarified.  If they're worth keeping
> > then it's worth someone blowing them up, Dr. Evil style.
>
> > A
>
> > On 11 February 2010 22:26, Kelly Wanser <[email protected]
> > <mailto:[email protected]>> wrote:
>
> >     A number of recent high caliber dicussions of Solar Radiation
> >     Management research, governance and deployment have focused
> >     exclusively on stratospheric aerosol dispersal. It may be useful
> >     for any who are thinking about solar radiation management to
> >     include tropospheric techniques, particularly the (relatively)
> >     mature proposed method of SRM via Marine Cloud Brightening
> >     (Latham-Salter technique) in policy and research considerations.
>
> >     There are important reasons to include marine cloud brightening as
> >     a component of any SRM research program.
>
> >        1. *The global cooling potential may be similar to
> >           stratospheric aerosols*. More work is needed, but early
> >           studies by Latham et. al. and more recent studies from Rasch
> >           et. al. and Caldeira et.al <http://et.al/>. indicate
> >           potential cooling/ CO2 offset effects and ice retention that
> >           compare favorable to forecasts for stratospheric aerosols.
> >        2. *The primary risk profile is different from stratospheric
> >           aerosols. *The techniques have differing precipitation
> >           effects and atmospheric chemistry.
> >        3. *The deployment profile is different. *Marine cloud
> >           brightening supports local /regional testing and deployment
> >           possibilities vs inherently global distribution in the
> >           stratosphere.
> >        4. *The duration of the effect is different. *Marine cloud
> >           brightening has a 2-3 day dissipation of the effect vs
> >           months or years for stratospheric aerosols.
> >        5. *The research profile is different. *Cloud-aerosol dynamics
> >           are an important gap in atmospheric science and cloud
> >           models, and aspects of early research in marine cloud
> >           brightening are similar or identical to studies of these
> >           general questions.  In addition, it is possible to study
> >           engineered effects on cohorts of clouds or regions of
> >           climate in a way that is difficult or impossible to do in
> >           the stratosphere.
> >        6. *Policy and public perception are different.* Local or
> >           regional cloud-aerosol research is likely to have fewer
> >           international regulatory considerations and a more benign
> >           public perception.
> >        7. *Experience and knowledge transfer*. There is likely to be
> >           very useful knowledge sharing across teams working on
> >           scientific, modeling and technical issues for both the
> >           stratosphere and the troposphere which should lend to more
> >           rigor, transparency and better informed regulation and
> >           monitoring of each.
> >        8. *Inadvertent tropospheric/cloud brightening effects are
> >           already occurring*, and require additional research.  Large
> >           scale reduction in emissions may have warming effects in
> >           which albedo offset alternatives may be desirable.
> >        9. *The optimum approach may be to use multiple techniques*.
> >           The risk-benefit profiles of the two most mature methods of
> >           solar radiation management, stratospheric aerosol dispersal
> >           and marine cloud brightening, suggest the possibility that
> >           the use of multiple sources of radiative forcing may reduce
> >           overall side-effects.
>
> >     A large collaborative effort is underway that includes researchers
> >     at Manchester University, Leeds University, the University of
> >     Washington, the University of Edinburgh, NCAR, PNNL, PARC, Purdue
> >     University and elsewhere, to continue to analyze cloud aerosol
> >     effects in marine clouds and their impact on climate. This
> >     research will advance both understanding of currently poorly
> >     understood dynamics in the climate system (clouds and aerosols,
> >     boundary layer effects etc) and to advance knowledge relevant to
> >     marine cloud brightening as a form of geoengieering.
>
> >     Kelly Wanser
> >     Silver Lining Project
>
> >     --
> >     --
> >     Kelly Wanser
> >     CEO
> >     eCert, Inc.
> >     One Market Street, Suite 3500
> >     San Francisco, California 94105
> >     p. +1 (415) 734-6790
> >     f. +1 (415) 651-8932
> >     e. [email protected] <mailto:[email protected]>
>
> >     eCert - Trust the Message
> >    http://www.ecertsystems.com
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