Table 1 List of experimental design aspects.

From: Overestimated climate warming and climate variability due to spatially homogeneous CO2 in climate modeling over the Northern Hemisphere since the mid-19th century

Experiment name

Short name

Time control

CO2 concentration

Control run

CTL

1–1250 (model year)

Fixed at 284.7ppmv everywhere

Spatially inhomogeneous CO2 runs

SIC runs, members:

SIC228, SIC483, SIC630

Branch runs starting from 228th, 483td, and 630th years, lasting for 150 years

Dynamic CO2 concentration with spatial differences, derived from the NCAR dataset28

Spatially homogeneous CO2 runs

SHC runs, members:

SHC228, SHC483, SHC630

Branch runs starting from 228th, 483td, and 630th years lasting for 150 years

Dynamic but spatially homogeneous CO2 concentrations, keeping yearly global mean atmospheric CO2 concentration exactly the same as the corresponding SIC runs