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The abstract is also wrong about energy consumption. Photosynthesis is inefficient. If one percent of the light goes into biomass it is doing well. You also need to account for the inefficiency of generating light. So at best you need a hundred times as much energy as you would get out of carbon in the first place. Even the worst of air capture is better than that.
All told this is a huge boondoggle. It is bad for the environment, it consumes ridiculous amounts of energy, and as a result it is hugely expensive.
Klaus
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In any case perhaps with some adjustment the idea may have merit. How about lighting desert plantations in marginal areas, not in pristine forest where delicate flora and fauna exist. Solar power can recharge batteries or lighting. Or extreme northern boreal forest, where few other animal forest species exist in large numbers. In areas of low radiation such a light boost may be just what it takes to increase productivity.
Oliver
-- Dr. Oliver Branch Inst. for Physics and Meteorology (120) University of Hohenheim Garbenstr. 30 D-70599 Stuttgart phone: 0711 - 459 -23132
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On Nov 10, 2021, at 12:55 PM, Oliver <oliver...@uni-hohenheim.de> wrote:
Do you not think this is rather a kneejerk reaction? Is it as awful an idea as injecting thousands of tons of silver dioxide or similar materials into the stratosphere? An action which will influence the global weather for a minimum of 4 years if done at the equator. Now that is a truly awful idea. On the other hand, I would say that the consequences of lighting forests are more predictable, and the idea is scalable and can be stopped easily.
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Hello Michael,
Absolutely agreed on your point about rich desert ecology, and
that we need to be humble in the face of the complex earth system.
In all likelihood, all goeengineering methods are in some way
'simplistic' because they intervene in processes which have
evolved over time, in symbiosis with the Earth system's changing
state, as driven from the outside by Milankovich cycles and
tectonic processes.
However, we are at the point now where we are looking for 'least
worst' solutions rather than magic bullets which moderate global
forcing with little impact on important ecosystem services, as
they probably don't exist. Hence, there is a risk calculation
where we may need to accept a limited amount of damage to achive
the greater good, i.e., a reduction in glocal forcing to preserve
as many ecosystems as possible. Saving every desert ecosystem with
little biomass may be a luxury we cannot afford.
Furthermore, I would argue that we need to shift away from a
'magic bullet' geoengineering paradigm to one which advocates a
diverse mix or 'package' of smaller scale solutions which all
together have a synergetic impact on forcing, e.g., a mixture of
regional aforestation, white roofs, marine cloud brightening,
cirrus thinning, enhanced weathering, CCS and so on (these must be
scaleable, sustainable and quickly reversible). By doing this, we
retain the option to assess these pathways and then emphasize or
deemphasize individual options over time as their impacts on
society and environment become apparent.
In consequence, one must redefine 'geoengineering' in a way that
removes the requirement that any one single method needs to have a
measurable impact on global forcing. An example of this is instead
is to call methods 'regional geoengineering'. We would also need
to refine our notion of what success is for these solution. In
other words, a reduction in forcing of 0.01 W m-2 might be called
a success, instead of requiring 0.2 W m-2 or similar as a
benchmark (arbitrary numbers). Research would need to reflect
this complex mix instead of writing paper after paper on the
impacts of e.g. global reforestation alone, or global SAI alone,
and so on.
However, in my opinion SAI should be thought of in a different
catgory to geoengineering. Recreating Pinatubo or Krakatoa is
neither scaleable, or easily reversible and hence gives the rest
of geoengineering proposals a bad name. On the other hand, marine
or cirrus cloud seeding and its meteorological impacts can be
stopped much more rapidly (of course, feedbacks with vegetation
may be much slower).
Regards
Oliver
-- Dr. Oliver Branch Inst. for Physics and Meteorology (120) University of Hohenheim Garbenstr. 30 D-70599 Stuttgart phone: 0711 - 459 -23132
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On Nov 10, 2021, at 10:52 PM, Ernie Rogers <ernie.e...@gmail.com> wrote:
Any option involves pros and cons, but it is curious to refer to SAI as neither scalable nor reversible. For scalability, it is essentially the only option we know for sure can scale (as your own email suggests by choice of defining success). For reversibility, if you stop putting aerosols in, the effect goes away. Note that if you’ve been doing it long enough for it to matter, then the time constant of the effect going away is going to be mostly dominated by the response times of the climate system, not by the residence time of the aerosols. So it’s true that the termination shock would be a bit more abrupt for MCB than for SAI, but that’s probably not that big a deal. It would seem to me that if one wants to do a comparison between methods, then one ought to actually evaluate their impacts rather than arbitrarily dismissing them by throwing incorrect adjectives around.
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