investigated using simulations from 12 Earth System models contributing to the
Geoengineering Model Intercomparison Project (GeoMIP). We contrast an idealized
experiment, G1, where the global mean radiative forcing is kept at preindustrial conditions
by reducing insolation while the CO2 concentration is quadrupled to a 4× CO2 experiment.
The reduction of evapotranspiration over land with instantaneously increasing CO2 …