Not exact matches
For these types of
radiative climate forcings the atmospheric temperature profile will be shifted basically unchanged to its
new equilibrium position.
Actually to reach a
new, higher
equilibrium temperature, the Earth surface (including oceans) must warm and thus the
radiative budget MUST be unbalanced, less radiation must be emitted in space compared to the (unchanged) incoming solar radiation.
It's just fundamental physics that this large
radiative forcing must result in global warming until the Earth reaches a
new energy
equilibrium at a higher temperature.
Anything by which we could delay the
radiative output for a while, up to a
new equilibrium, with constant input from the sun, would suffice (Q - out < Q - in).