| This simulation estimates potential global change using
a coupled climate model that has interactive atmosphere, ocean, land,
and sea ice components.
A control climate was established by running the model for over
70 years with solar forcing and greenhouse gases held at present
day levels. Two additional experiments were then performed, one
of which has expected increases in greenhouse gases, such as carbon
dioxide, and another, in which the additional effects of sulfate
aerosols are included.
The differences from the control for a running average of the
Dec/Jan/Feb surface air temperature are shown in the next sequences
which span over 70 years into the future. Note that some regions
experience cooling relative to the control experiment, and other
areas have less warming than with increasing greenhouse gases alone.
Temperature and albedo differences are represented as shown below
for a running average of the means of Dec/Jan/Feb. |