Dear Mike,

Yes, I agree we have barely scratched the surface for the number of
strat/particle scenarios we need to test.

Sincerely,

Oliver Wingenter

On Jan 13, 7:38 pm, Mike MacCracken <[email protected]> wrote:
> Dear Andrew and Tom--
>
> While the preindustrial temperature might be right for preserving/restoring
> Greenland and sea level, society has likely adapted to the conditions of the
> past several decades, so going back to the 19th century would likely lead to
> quite dramatic impacts to agriculture, killing frosts in many areas now
> being farmed, etc. I would think the world decision would thus likely be at
> a level somewhere between value in 1950 and about 1990. In any case, the
> transition to such a temperature range should likely be sort of gradual and
> not sudden--rapid changes cause increased impacts.
>
> I would also suggest that we no one has yet done any tests on having more
> aerosols in one season than another. The average will likely be what
> controls ocean temperatures, but land temperatures can be significantly
> affected, so maybe focus on limiting summer warming and keep winters a bit
> warm. From the orbital element results, to build up glaciers and ice sheets,
> what we want is cool summers and warm winters (so there is more
> snowfall)--of course, there is a lot of checking to do about how the
> monsoons would be affected, etc.
>
> There is also the issue of latitudinal distributions. There are far more
> than the two choices that have been simulated, namely global and Arctic
> only.
>
> So, I would hold off on the idea of a single temperature change or goal--if
> we are going to take control of the climate through geoengineering, we can
> be subtle in our efforts, correcting the worst aspect of the changes, if not
> all. Thus, I'd tend to agree that ultimately, there is going to have to be
> some quite extensive consideration of what might be done.
>
> Best, Mike MacCracken
>
> On 1/13/09 9:17 PM, "Andrew Lockley" <[email protected]> wrote:
>
>
>
> > Bearing in mind that we're still unsure as to the various feedback
> > effects, shouldn't the default position be that we should plan to go
> > back to pre-industrial temperatures.  Anything that we can later show
> > is not needed is then a 'free gift' in terms of effort we don't need
> > to expend.  The alternative could be that we suddenly have to ramp up
> > our efforts at the last minute when we realise that we've forgotten
> > some deadly feedback.  That seems like a bad way of planning.
>
> > A
>
> > 2009/1/14  <[email protected]>:
>
> >> Dear all,
>
> >> This is a non issue as it is already covered by Article 2 of the
> >> UNFCCC. The global-mean temperature at which we should seek to
> >> stabilize, vide Article 2, is one that avoids "dangerous anthropogenic
> >> interference with the climate system" (etc., etc.) Whether we
> >> stabilize the climate through mitigation (Kyoto Protocol), geoengineering,
> >> or combined mitigation/geoengineering, the issue is the same.
>
> >> It is true that "dangerous interference" is not well defined, but
> >> there is a large literature on this.
>
> >> The main difference between stabilization via mitigation or via
> >> geoengineering is one of timescale. With mitigation there are two main
> >> timescales, that associated with the carbon cycle and the slow response
> >> of concentrations to emissions changes, and that associated with the
> >> thermal inertia of the oceans. With geoengineering, the first timescale
> >> is virtually eliminated (which might be seen as an advantage - see below).
> >> The second timescale is common to all climate stabilization methods.
>
> >> Furthermore, there are two major sources of uncertainty in both cases.
> >> In mitigation, there is uncertainty in relating emissions changes
> >> to radiative forcing, and uncertainty in relating forcing to equilibrium
> >> response (associated with climate sensitivity uncertainties). With
> >> geoengineering, there is uncertainty in relating injection rate of
> >> sulfur into the stratosphere to forcing, and the same climate sensitivity
> >> uncertainty. The parallels are clear and obvious.
>
> >> Eliminating the first response time with geoengineering is, at first
> >> blush. a big advantage. (Of course, we could do something similar with
> >> mitigation, at least partly, by, e.g., reducing CH4 levels -- where the
> >> timescale for concentration response is much less than for CO2, but we
> >> cannot solve the problem with CH4 alone.)
>
> >> This response time issue has been addressed in the mitigation case in
> >> the paper noted below. Here, we consider the issue of changing course,
> >> in, e.g., the case where we decide on a stabilization level (say 550
> >> ppm) and then realize that we need a much lower level (e.g. 350 ppm).
> >> With mitigation this is a tough call, because of inertia in the carbon
> >> cycle. With geoengineering we would have a much better chance of saving
> >> the planet from doom should we suddenly realize that the proposed
> >> stabilization target was too high. Geoengineering might give us control
> >> that we can never get with mitigation.
>
> >> Please excuse my ramblings here. My main point is that the issue of
> >> what temperature to dial simply does not have to be considered any more
> >> than it is or has been already. It is already covered by Article 2.
> >> Perhaps not well covered -- but this is not a new problem.
>
> >> Tom.
>
> >> +++++++++++++++++++++++++++++++
>
> >> Wigley, T.M.L., Richels, R. and Edmonds, J.A., 2007:  Overshoot pathways
> >> to CO2 stabilization in a multi-gas context. (In) Human Induced Climate
> >> Change: An Interdisciplinary Assessment (eds. Michael Schlesinger, Haroon
> >> Kheshgi, Joel Smith, Francisco de la Chesnaye, John M. Reilly, Tom Wilson
> >> and Charles Kolstad), Cambridge University Press, 84­92.
>
> >> +++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++
>
> >>> Dear Group,
>
> >>> The question of what temperature to "dial" in the Earth could also an
> >>> important topic this proposed group could discuss and possibly decide
> >>> on.
>
> >>> Oliver Wingenter
>
> >>> On Jan 12, 6:24 pm, "Andrew Lockley" <[email protected]> wrote:
> >>>> No Oliver, I do think what's needed is an international Board of great
> >>>> scientists and engineers.  Whilst this body develops, I see an interim
> >>>> Board composed of members of this group as a useful stepping stone.
> >>>> However, you should note that I've already asked people to think of
> >>>> non-googlegroup members who can contribute in order to 'raise the
> >>>> game'. I certainly never thought for a moment that it should be
> >>>> 'closed' to non-googlegroup people!
>
> >>>> Some of the initial members drawn from this googlegroup would probably
> >>>> remain on this Board as it developed into a high-level panel, as this
> >>>> googlegroup currently includes World-class scientists.  Others
> >>>> members, such as myself, would probably step down as the Board took on
> >>>> other members.
>
> >>>> A
>
> >>>> 2009/1/13 Oliver Wingenter <[email protected]>:
>
> >>>>> Dear Andrew,
>
> >>>>> I think our plans are for different types of panels or boards.
> >>>>> Correct me if I am wrong but yours would be comprised exclusively of
> >>>>> Google geo members for the purpose of ranking project with yourself
> >>>>> included so as to aid casual wiki users.  Some projects are still in
> >>>>> their infancy.
>
> >>>>> My notion is for an international panel comprised of scientist from
> >>>>> many disciplines that can approve or endorse geoengineering projects
> >>>>> nearly ready for deployment.  Oversight is needed to avert possible
> >>>>> eco disasters.
>
> >>>>> We may first want have an international committee whose sole purpose
> >>>>> is to seat a permanent committee.
>
> >>>>> I am not proposing to take the lead.  Some of Ken's stature is
> >>>>> required.
>
> >>>>> Sincerely,
>
> >>>>> Oliver Wingenter
>
> >>>>> On Jan 12, 4:32 pm, "Andrew Lockley" <[email protected]> wrote:
> >>>>>> (I endorse John's comments.)
>
> >>>>>> We won't all agree, but we do need to move forward together with
> >>>> broad
> >>>>>> consensus.  At the moment we seem to have about a 50% split between
> >>>>>> supporters and opposers.
>
> >>>>>> The way I see it we now have 4 choices for progressing the Board, and
> >>>>>> the discipline as a whole.
>
> >>>>>> 1) We do nothing, relying on the 'current process' (whatever that is)
> >>>>>> to deliver any necessary geoeng in time.  I personally don't believe
> >>>>>> there's currently enough scrutiny and oversight to encourage
> >>>>>> politicians to take prompt action.
> >>>>>> 2) The volunteers set up the Board in defiance of those people who
> >>>>>> oppose such a move.  This strikes me as divisive.
> >>>>>> 3) The opposers could come up with a list of changes or rules they'd
> >>>>>> need to see before they can support the board.  This seems sensible,
> >>>>>> if people are willing to do this.
> >>>>>> 4) Someone can come up with a better idea, which we all do instead.
> >>>>  I
> >>>>>> am sure there are some good ideas out there.
>
> >>>>>> Whilst I accept that not everyone will agree with whatever we decide
> >>>>>> to do, I would like to think that people can at least be positive and
> >>>>>> help the group make a decision that is supported by most people.  I'd
> >>>>>> also like to see people being respectful of everyone's opinion and of
> >>>>>> the offer the volunteers have so kindly made.
>
> >>>>>> A
>
> >>>>>> 2009/1/12 John Nissen <[email protected]>:
>
> >>>>>>> Hi all,
>
> >>>>>>> I see a lot of negative comment to Andrew's suggestion.
>
> >>>>>>> But supposing somebody finds strong evidence that the Arctic sea
> >>>> ice is very
> >>>>>>> likely to disappear (at end summer) in two or three years, where
> >>>> does he
> >>>>>>> go?  Don't we need a body of people who can say - well - there are
> >>>> these
> >>>>>>> particular geoengineering techniques that have a good chance of
> >>>> helping to
> >>>>>>> save the Arctic sea ice?  As Ken said, there is no alternative to
> >>>>>>> geoengineering for
>
> ...
>
> read more »
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