Not exact matches
Corresponding time for surface + tropospheric
equilibration: given 3 K warming (including feedbacks) per ~ 3.7 W / m2 forcing (this includes the effects of feedbacks): 10 years per heat capacity of ~ 130 m layer of ocean (~ heat capacity of 92 or 93 m of liquid
water spread over the whole globe)
Across the world's oceans there is a continual cycle of
equilibration of dissolved carbon dioxide in
water with carbon dioxide in the atmosphere.
As you equilibriate, the planet warms (reducing the TOA imbalance) and
water vapour increases, increasing the amount of surface LW absorbed in the atmosphere, but not adding to the TOA imbalance (though it does slow the
equilibration).