Dear Ken,

I agree. Testing nozzles or testing flying one plane into the stratosphere to see if you can create sulfate aerosols is OK with me. But a planned campaign spanning hundreds of km, and weeks to months, is something that needs informed consent or environmental impact statements first.

And we also need to clearly define what the line is between these two, and that determination needs to be based on science and on model results. Nobody has determined yet how you draw the line between nozzle testing and a field experiment. What are the time, space, and injection amount values that could be permissible now? And how does society decide this?


Alan

Alan Robock, Professor II (Distinguished Professor)
  Editor, Reviews of Geophysics
  Director, Meteorology Undergraduate Program
Department of Environmental Sciences        Phone: +1-732-932-9800 x6222
Rutgers University                                  Fax: +1-732-932-8644
14 College Farm Road                   E-mail: [email protected]
New Brunswick, NJ 08901-8551  USA      http://envsci.rutgers.edu/~robock


On 10/2/2010 1:29 PM, Ken Caldeira wrote:
Alan,

While you may be correct that there is no hurry to spray salt into clouds, and there may be good reasons to delay testing nozzles in the field, guaranteeing "that you will be able to measure a signal and test all possible benefits and risks" should not be a pre-condition to all tests.

What if somebody is just trying to test whether a nozzle works, and there is absolutely no expectation of any harm (i.e., you are just spraying a little seawater into the air)?

What dangers are you guarding against? The scale of environmental interference would be orders of magnitude smaller than produced by most ships burning high sulfur fuels.

It is just silly to act as if these kind of experiments bear significant direct environmental risks.

The motivations for delay are largely socio-political, related to the need for governance and control, and not because there is any expectation of significant risk or harm from the specific experiment.

A more direct example is that Matthew Watson of Bristol is apparently planning to test the "hose to the sky idea", but apparently planning to pump water instead of sulfur.

http://www.theengineer.co.uk/news/news-analysis/particle-injection-could-abate-climate-change/1003647.article

Are we to say that nobody can pump water up a hose to a balloon without guaranteeing "that you will be able to measure a signal and test all possible benefits and risks"?

I think we will be seeing a number of geoengineering tests proposed where there is no expectation of direct harm, and it will be very difficult to know how to regulate such experiments.

Can nobody do any tests that involve pumping liquids to dirigibles? Or is it only if those tests are "geoengineering-related"? What if the funder is interested in commercial applications but the scientists are interested in geoengineering? What if the situation was reversed and the scientists have no geoengineering-related intent? And so on and so on.

Part of keeping this conversation clear is to be clear about whether we are worried about (1) direct environmental risks from a particular experiment or we are worried about (2) socio-political risks stemming from an experiment [i.e., it might spur an inappropriate regulatory backlash] or (3) risks from possible future scale-up to which an experiment could potentially lead.

For most of the small-scale tests being discussed today (e.g., testing nozzles, etc), the concerns fall into categories 2 and 3. For these experiments, we should not pretend that the experiment itself is likely to present real and significant direct environmental risk.

Best,

Ken
___________________________________________________
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA
+1 650 704 7212 [email protected] <mailto:[email protected]>
http://dge.stanford.edu/labs/caldeiralab  @kencaldeira


On Sat, Oct 2, 2010 at 6:22 AM, Alan Robock <[email protected] <mailto:[email protected]>> wrote:

    Dear Mike,

    Thanks for the update on the models.  This makes an even stronger
    case for model experiments before we go out into the field.  We
    really need to understand what the potential reactions will be to
    cloud seeding so we can guard against dangers and so that we can
    design field experiments that have the potential to teach us about
    how the system works.  I can see no argument to hurry up and go
    spray salt into clouds now without a sound theoretical background
    to guide where and for how long to spray, to guarantee that you
    will be able to measure a signal and test all the potential
    benefits and risks.  Current arguments to go do this as soon as
    possible lack such modeling backgrounds, that I know of.


    Alan

    Alan Robock, Professor II (Distinguished Professor)
       Editor, Reviews of Geophysics
       Director, Meteorology Undergraduate Program
    Department of Environmental Sciences        Phone: +1-732-932-9800 x6222
    Rutgers University                                  Fax: +1-732-932-8644
    14 College Farm Road                   E-mail:[email protected]  
<mailto:[email protected]>
    New Brunswick, NJ 08901-8551 USA http://envsci.rutgers.edu/~robock
    <http://envsci.rutgers.edu/%7Erobock>


    On 9/29/2010 12:13 PM, Mike MacCracken wrote:
    Yesterday I got to visit the NOAA lab in Boulder and, among other things,
    get to see the simulations being done by their 15 km resolution icosahedral
    grid simulation model with a finite volume numerical scheme. Other physics
    is from the plug-in packages that are available and used in other GCMs. They
    are running 10 day forecasts twice a day, and the results certainly look
    quite good--better resolution really does help make things appear, at least
    with respect to viewing of satellite movies of how the real world is
    looking. And they are now getting to explore addition of the smaller scale
    aspects not now represented in GCMs (at some point, the heat emissions from
    energy use will become important for urban regions; reasonable up slope and
    down slope flows; etc.)

    With respect to the proposed experiments, it is true that the weather is
    chaotic (that is, changing the least significant bits in the initialization
    of the model does over a couple of weeks lead to randomly correlated
    weather), and that is what Alan is talking about for the weather time scales
    (for climate scales, that requires longer simulations and experiments). But,
    at the high resolutions that will soon be available (they are aiming in 1-2
    years for 4 km non-hydrostatic model, depending on timing of next generation
    of graphical processors), my guess is that it is going to be possible to
    explore the types of changes in weather that might result as a consequence
    of the early cloud brightening field experiments. It will likely require an
    ensemble set of simulations (things already being explored in simulations
    with and without aerosols, etc.).

    As these models get more and more refined and seem to simulate more and more
    phenomena that have previously been considered part of the variability [we
    should really be saying unexplained instead of natural (even chaotic)
    variability until we really get to better models], there will be more and
    more capabilities to determine the significance of the changes in models,
    and by thoughtful planning of the experiments, in the observations.

    Mike


    On 9/29/10 5:16 AM, "Stephen Salter"<[email protected]>  
<mailto:[email protected]>  wrote:

       Hi All

    Alan says that climate signals will be drowned out by chaotic climate
    variations.  Both the papers that I pointed to in my email of 24
    September were about picking up small signals from large, random
    variations.   The second paper suggests that a 20 year run of the
    pseudo-random stimulus idea might be able to detect changes which are
    one or two percent of the root mean square of the  natural variation. I
    am still hoping for suggestions.

    If I knew a bit more about chaos I would like to argue whether or not
    the climate is chaotic or we are just ignorant about climate.  The best
    scientists and philosophers used to think that planetary motions, the
    behaviour of chemical elements and the incidence of infectious illnesses
    were chaotic.  Believing that something is chaotic is an excellent way
    of never discovering useful things about it.

    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
    Mobile 07795 203 195
    www.see.ed.ac.uk/~shs  <http://www.see.ed.ac.uk/%7Eshs>


    On 28/09/2010 20:44, Douglas MacMynowski wrote:
    Alan - I doubt there's any real disagreement here, but just a
    clarification; climate variability/noise is irrelevant to the question
    of whether some form of SRM can be tested, but of course critical to
    the question of how long it would take to detect a signal.  If the
    goal is to estimate changes on a global scale, that will take decades
    and significant forcing levels (we have a paper under review on this
    subject that puts numbers on that trade-off).  Other than the moral
    hazard, I see no basic difference between testing this, and any other
    experiment in any other field of engineering or science.  Clearly with
    one Earth, I agree with learning everything we can with computer
    testing first, but if we ever did want to do this in full-scale, I'd
    rather start small and learn something rather than just turning it on
    and hoping for the best.

    doug

    On Sep 27, 11:44 am, Alan Robock<[email protected]>  
<mailto:[email protected]>   wrote:
        Dear Ken,

    I think you are being rather picky with words.  In any case, I never
    said it cannot be tested.  I said it cannot be fully tested in a
    real-world in situ experiment without full-scale implementation, because
    the climate signal will be drowned out by chaotic climate variations and
    because injecting into a pristine stratosphere cannot test injecting
    into an existing cloud.  Of course computers can be used for testing.
    That is what I do, and I advocate much more of it.  The statement below
    refers to in situ experimentation.

    Alan

    Alan Robock, Professor II (Distinguished Professor)
         Editor, Reviews of Geophysics
         Director, Meteorology Undergraduate Program
    Department of Environmental Sciences        Phone: +1-732-932-9800 x6222
    Rutgers University                                  Fax: +1-732-932-8644
    14 College Farm Road                   E-mail:[email protected]  
<mailto:[email protected]>
    New Brunswick, NJ 08901-8551  USAhttp://envsci.rutgers.edu/~robock  
<http://envsci.rutgers.edu/%7Erobock>

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