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The projected temperature changes are always presented as simulated changes relative to the simulated temperatures of the individual models for the baseline period 1961 1990.
Table 1 shows the simulated changes between 2006 and 2025.
The magnitude of simulated changes using the SLAMM was 46% of reference changes.
Qian et al. ([2011]) simulated changes in Ti in response to doubling CO2 during solar minimum conditions.
Gavrilov et al. (2013b) simulated changes in the amplitudes of atmospheric planetary waves (PWs) caused by stationary OGWs.
There have been significant LCC, where urban land covered 21.4 % of simulated changes in 2011 and 37.4 % in 2025.
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This increase in the latent heat flux was higher than the simulated change in rainfall in the WPH region.
To do this, participants are first sorted by their simulated change, from smaller to larger (line 5).
For each attractor, and for each perturbed gene, we registered whether a qualitative change is produced or not, and the final attractor attained after the simulated change.
The model's response to a simulated change in the environment was investigated by doubling the level of one uncompensated factor.
We calculate the simulated change in each variable using the ensemble mean of that variable in the baseline and future periods.
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