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a near-zero pre-industrial background concentration,
primarily due to human activities. {WGI 2.3, SPM; SROC SPM}
There is very high confidence that the global average net
effect of human activities since 1750 has been one of warm-
ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2
(Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM}
The combined radiative forcing due to increases in CO2, CH4
and N2O
/media/loftslag/IPPC-2007-ar4_syr.pdf
....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
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Exampl
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
of how climate change will
impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources
and taking advantage of the local tempered climate for keeping the
supercomputer components cool, the running costs and CO2 footprint
will be kept to a minimum, saving tonnes of CO2 in line with the
four nations' efforts towards reaching Net/about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
at
e
(C
limat
e
models
)
GC
M
s
X
X
XX
X
X
X
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RCM
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X
XX
X
X
X
X
Initia
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riabilit
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X
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/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
Fi
g.
1
O
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Public Choice (2012) 151:91–119 99
Table 1 The predicted effect of
intrinsic preferences on first and
second movers’ contributions
1st mover 2nd mover
Disadvantageous Negative None
inequity aversion
Advantageous None Positive
inequity
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf