http://implicc.zmaw.de/

IMPLICC - Implications and risks of engineering solar radiation to limit
climate change

IMPLICC addressed the call ”Implications and Risks of Novel Options to
Limit Climate Change“ within the activity "Climate Change, Pollution and
Risks” of the European Union's framework-7 programme (FP7) for research,
technological development and demonstration activities (2007-2013). The
project was running from July 2009 until September 2012 under the
cooperation of 5 higher educational and research institutions in France,
Germany and Norway. The overall activities of the project are coordinated
by the Max Planck Institute for Meteorology in Hamburg. The final
scientific report for the project will be posted on this site once it is
accepted by the European Commission. A "Synthesis report for policy makers
and the interested public" can be found here. Many of the numerical climate
simulations performed within IMPLICC have followed
the GeoMIP (Geoengineering Model Intercomparison Project) protocol. The
results of those simulations are available via the Earth System Grid (ESG).
For more information on results of the project and ongoing research
activities, please contact the project participants.



Brief summary of scientific results

Within the IMPLICC project, five partner institutes from France, Germany
and Norway have studied the effectiveness, side effects, risks and economic
implications of climate engineering through different solar radiation
management techniques suggested to limit climate change. The main tools
used in these studies were state-of-the-art numerical Earth system models
(in some cases augmented by specific treatments of atmospheric aerosols and
chemistry) and an economic model. One central question was what climate
would result from the application of three different CE techniques: the
reduction of solar irradiance (through space mirrors); the enhancement of
the reflection of solar radiation through stratospheric sulfate aerosols;
and the manipulation of marine clouds through injection of sea salt. One
novel aspect of IMPLICC in the context of climate engineering research was
the implementation of a model intercomparison study in order to identify
robust climate response patterns.In an idealized experiment with large
greenhouse gas forcing balanced globally by the reduction of solar
irradiance it was shown that it may be possible to compensate the increase
of global mean temperature. However, the increase in global total
precipitation that is expected in scenarios with enhanced greenhouse gas
concentrations would be overcompensated by solar radiation management: a
geoengineered climate would have less precipitation than a natural climate
of the same global mean temperature. The model intercomparison showed that
precipitation decreases – under the chosen scenarios - would particularly
affect large land masses in the mid-latitudes of the Northern hemisphere,
i.e. Canada and the US, central and northern Europe and Asia.The simulation
of a scenario with a much smaller degree of geoengineering, where just the
increase of climate forcing through a moderate greenhouse gas emission
scenario after the year 2020 would be compensated, showed, not
surprisingly, a much smaller climate impact. Because of the weakness of the
forcing, the regional patterns of the simulated responses are also less
robust than under strong forcing. It was, however, clearly shown that an
abrupt termination of climate engineering efforts would lead to very rapid
climate change.The estimation of economic implications of climate change
and climate engineering on long time-scales has obvious limitations.
However, our simulations suggest that additional climate engineering under
a moderate mitigation scenario may not be economically advantageous. This
could be different under high-emission scenarios, but also it is then
unclear if the economic importance of side-effects would become
significant.IMPLICC has also made progress on microphysical processes
involved in the aerosol-based radiation management methods, which help
determine their effectiveness. It has become clear that the effectiveness
of the methods depends strongly on the implementation, e.g. on the size of
emitted sea salt particles. However, uncertainties concerning the amount of
aerosol necessary to reach a certain climate effect remain.It has become
clear during the course of the project that some of the remaining
uncertainties concerning implications of climate engineering are caused by
limited understanding of climate processes in general, which are not
necessarily specific to climate engineering. The manipulation of marine
clouds, for example, is based on aerosol-cloud interaction processes which
are one of the big open questions of climate research, independent of the
origin of aerosols. Injecting sulfur into the stratosphere would not only
have radiative but also dynamical effects. Dynamical
stratosphere-troposphere coupling would need to be better understood in
order to fully appreciate the effects of such climate engineering.Finally,
it needs to be noted that the climate response is only one aspect that has
to be considered when the implementation of climate engineering techniques
is discussed. Other potential side effects specific to some methods, as
well as political, ethical, legal and further economic implications have to
be taken into account. But the potentially strong climate responses
discussed here suggest that climate engineering cannot be seen as a
substitute for a policy pathway of mitigating climate change through the
reduction of greenhouse gas emissions.

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