Previous: Model description Next: Discussion Up: Ext. Abst.
2. Experiment design
Our experiment aims at investigating the effects of enhanced solar
UV radiation on climate. For this purpose, 2 separate runs of
the model are being performed, lasting for 20 model years. The
first model run represents conditions prevailing at the state
of maximum solar activity during the sun's 11-year cycle, with
enhanced solar irradiance mainly at the UV intervals, while the
second run represents minimum solar activity conditions.
The basic state of the model, an 'average' state of the 11-year
solar cycle, is a simulation of the present-day atmosphere, representing
a time-slice for 1990, with carbon dioxide concentration set to
353 ppmv and chemical boundary conditions for 1990. The Sea Surface
Temperature (SST) is fixed in the model, representing a 1974 -1994
climatology. The runs are performed from re-start files from a
60-year model run.
The solar fluxes in both perturbation runs were adjusted in the
model's spectral intervals according to the difference between
the solar minimum and solar maximum spectral solar flux changes
(Lean et al., 1997). The changes are summarised in Table 1. Maximum
solar activity is represented by enhanced solar flux distributed
within the radiation scheme spectral intervals and enhanced solar
flux distributed at the wavelength bands used for the photolysis
rate calculations.
Table 1. Changes in Solar Flux
(* The number in parenthesis is the fixed wavelength at each spectral
interval used in the photolysis rate calculation scheme. See Landgraf
and Crutzen, 1998, for details)