And a link to the referenced paper: 
http://link.springer.com/article/10.1007%2Fs00382-013-1761-5

"Until now, climate model intercomparison has focused primarily on annual and 
global averages of various quantities or on specific components, not on how 
well the general dynamics in the models compare to each other. In order to 
address how well models agree when it comes to the dynamics they generate, we 
have adopted a new approach based on climate networks. We have considered 28 
pre-industrial control runs as well as 70 20th-century forced runs from 23 
climate models and have constructed networks for the 500 hPa, surface air 
temperature (SAT), sea level pressure (SLP), and precipitation fields for each 
run. We then employed a widely used algorithm to derive the community structure 
in these networks. Communities separate “nodes” in the network sharing similar 
dynamics. It has been shown that these communities, or sub-systems, in the 
climate system are associated with major climate modes and physics of the 
atmosphere (Tsonis AA, Swanson KL, Wang G, J Clim 21: 2990–3001 in 2008; Tsonis 
AA, Wang G, Swanson KL, Rodrigues F, da Fontura Costa L, Clim Dyn, 37: 933–940 
in 2011; Steinhaeuser K, Ganguly AR, Chawla NV, Clim Dyn 39: 889–895 in 2012). 
Once the community structure for all runs is derived, we use a pattern matching 
statistic to obtain a measure of how well any two models agree with each other. 
We find that, with the possible exception of the 500 hPa field, consistency for 
the SAT, SLP, and precipitation fields is questionable. More importantly, none 
of the models comes close to the community structure of the actual observations 
(reality). This is a significant finding especially for the temperature and 
precipitation fields, as these are the fields widely used to produce future 
projections in time and in space."

Best wishes,

Simon

________________________________________________

Simon Driscoll
Atmospheric, Oceanic and Planetary Physics
Department of Physics
University of Oxford

Office: +44 (0) 1865 272930
Mobile: +44 (0) 7935314940

http://www2.physics.ox.ac.uk/contacts/people/driscoll
________________________________
From: [email protected] [[email protected]] on 
behalf of Simon Driscoll [[email protected]]
Sent: 01 August 2013 19:06
To: [email protected]
Subject: [geo] Geoengineering carries unknown consequences

The physicists out there may have already seen this short article: 
http://www.physicstoday.org/resource/1/phtoad/v66/i8/p8_s3 (also copied down 
below) which may be of interest to group members.

Best wishes,

Simon

+++

I read with interest David Kramer’s piece on geoengineering (Physics Today, 
February 2013, page 17<http://dx.doi.org/10.1063/PT.3.1878>). I must say, I am 
more alarmed by what the geoengineers in his report are proposing than by the 
climate changes that are taking place. I believe geoengineers are removed from 
scientific reality. They ignore the fact that the climate system and its 
components—clouds, hurricanes, and so forth—are highly nonlinear and thus very 
sensitive to the initial conditions and to changes in the parameters. 
Nevertheless, one could study the system’s response in a probabilistic way when 
certain parameters are changed or when we introduce fluctuations, if the 
relationships among all the components are known exactly.

And here lies the whole problem with geoengineering. The formulation of the 
climate system and its components is only approximately known. More than 30 
climate models are floating around in the climate community, and their 
predictions about general dynamics simply don’t agree with each other. In a 
recent 
publication,1<http://www.physicstoday.org/resource/1/phtoad/v66/i8/p8_s3#c1> we 
considered 98 control and forced climate simulations from 23 climate models and 
examined their similarity in four different fields (upper-level flow, sea-level 
pressure, surface air temperature, and precipitation). We found that except for 
the upper-level flow, the agreement between the models is not good. Moreover, 
none of the models compares well with actual observations.

One person in the Physics Today story said that geoengineering may result in 
changes in various weather patterns, but nobody knows what the changes are 
going to be and how they will affect the climate system. If the warming in the 
Arctic is a big event to mitigate, then it will require a significant 
“geoengineering” effort. To me, that means significant changes will occur 
elsewhere. Who can say whether those changes will be less serious than those 
taking place now? How can geoengineers talk about modifying clouds and albedo 
when clouds are represented in the climate models as mostly linear 
parameterizations?

Kramer’s report did not mention hurricanes, but geoengineers also propose to 
dissipate them. Hurricanes are unique in the climate system because they 
represent major self-organization. As physicists well know, self-organization 
occurs in dissipative systems in which energy is not conserved but instead is 
exchanged with the environment. Hurricanes involve huge amounts of energy. 
Scientists have little idea how the atmosphere and the ocean will be affected 
if that energy is not allowed to be exchanged.

I would not have a problem with geoengineering if the physics and dynamics of 
the climate system were well known. Climate scientists have a good idea of the 
large-scale flow of ocean currents, but detailed measurements are not 
available. They know the basic physics of cloud formation and its 
thermodynamics but do not fully understand detailed cloud microphysics or the 
complex connections between climate and ecosystems. And with complex nonlinear 
systems, details are important. So we need to make an effort to improve our 
understanding of our climate system and its components before we try to operate 
on it. We can engineer a car or a plane because we know the underlying physics 
of motion, combustion, and flight, and we understand the role of every 
component. Can geoengineers say the same about climate?

________________________________________________

Simon Driscoll
Atmospheric, Oceanic and Planetary Physics
Department of Physics
University of Oxford

Office: +44 (0) 1865 272930
Mobile: +44 (0) 7935314940

http://www2.physics.ox.ac.uk/contacts/people/driscoll

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