Evolving CO2 rather than SST accelerates GCM convergence by a factor of ten
Submitter
Romps, David — Lawrence Berkeley National Laboratory
Area of research
General Circulation and Single Column Models/Parameterizations
Journal Reference
Science
An earlier paper (Romps 2020) applied an inverse climate-modeling method to rapidly equilibrate SST and CO2 in limited-area cloud-resolving simulations and proposed a way to extend that inverse method to global climate models. Here, that approach is tested in a global aquaplanet simulation of perpetual equinox and is found to accelerate the equilibration by a factor of ten.
Impact
This speedup enables the equilibration of 51 climate simulations to measure, in fine detail, the bump in equilibrium climate sensitivity that has been reported around a global mean temperature of 310-320 K. Other potential applications include the ability to probe unstable climate states and climate states close to bifurcations, such as the runaway greenhouse transition.
Summary
Testing a proposal for rapid equilibration of global climate simulations finds a successful factor-of-ten speedup of climate simulations, enabling the probing of climate states not readily accessed via the standard slab-ocean methods.