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This experiment adds a fully interactive sulphur cycle to the model used in the climateprediction.net experiment.
This will help us to identify the effects of sulphate
aerosol on the global climate system and the sensitivity of the model to
perturbing sulphur cycle parameters.
For this new experiment, an extra 2 phases will be added
to the 3 phase experiment 1.
In one extra phase, the sulphate emissions will be changed to those expected in 2005,
and in the other both sulphate and carbon dioxide will be changed.
In addition, the sulphate emissions typical of 1985 will be included in the first 3 phases.
This experiment will be available for download for a limited period of time, just like the
thermohaline experiment
we ran in 2004.
Why do we want to include sulphate aerosol in our models?
Sulphates
act to scatter solar radiation and reduce the amount of solar energy reaching
the surface. The reduction in solar radiation cools the surface and reduces
the warming effect caused by greenhouse gases. So, a prediction of the
climate in the 21st century needs to contain the effects of sulphate aerosol
otherwise the warming trend may be overestimated - the so-called 'global dimming' effect.
From
this experiment it is hoped that we will be able to better understand the
range of uncertainty in climate models due to the parameters
in the sulphur cycle.
This information will then be used in climateprediction.net
experiments 2 & 3.
Figure 1 shows one model's surface temperature response to increasing sulphur emissions
from pre-industrial levels (natural) to present day levels (natural plus
anthropogenic). The cooling effect of sulphate aerosol can be seen throughout
the whole northern hemisphere and corresponds to the high sulphate burden
of the northern hemisphere shown in Figure 2.
Figure 2 shows the 1985 distribution of sulphate in the atmosphere over the
North Atlantic, North America and Europe. The regions of high anthropogenic
source emissions of sulphur dioxide leads to high concentrations of sulphate
aerosol over the northern hemisphere continents. Unlike greenhouse gases, the distribution
and concentration of sulphates varies a lot with location, as can
be seen by comparing the sulphate concentration over the North Pole with
that over North America.
Read about the experimental strategy of the standard, shorter experiment
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