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Equilibrium Climate Sensitivity Obtained From Multimillennial Runs of Two GFDL Climate Models
Author(s) -
Paynter D.,
Frölicher T. L.,
Horowitz L. W.,
Silvers L. G.
Publication year - 2018
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2017jd027885
Subject(s) - climatology , climate change , climate sensitivity , environmental science , climate model , inversion (geology) , general circulation model , atmospheric circulation , sea surface temperature , atmospheric sciences , geophysical fluid dynamics , geology , paleontology , oceanography , structural basin
Equilibrium climate sensitivity (ECS), defined as the long‐term change in global mean surface air temperature in response to doubling atmospheric CO 2 , is usually computed from short atmospheric simulations over a mixed layer ocean, or inferred using a linear regression over a short‐time period of adjustment. We report the actual ECS from multimillenial simulations of two Geophysical Fluid Dynamics Laboratory (GFDL) general circulation models (GCMs), ESM2M, and CM3 of 3.3 K and 4.8 K, respectively. Both values are ~1 K higher than estimates for the same models reported in the Fifth Assessment Report of the Intergovernmental Panel on Climate Change obtained by regressing the Earth's energy imbalance against temperature. This underestimate is mainly due to changes in the climate feedback parameter ( − α ) within the first century after atmospheric CO 2 has stabilized. For both GCMs it is possible to estimate ECS with linear regression to within 0.3 K by increasing CO 2 at 1% per year to doubling and using years 51–350 after CO 2 is constant. We show that changes in − α differ between the two GCMs and are strongly tied to the changes in both vertical velocity at 500 hPa ( ω 500 ) and estimated inversion strength that the GCMs experience during the progression toward the equilibrium. This suggests that while cloud physics parametrizations are important for determining the strength of − α , the substantially different atmospheric state resulting from a changed sea surface temperature pattern may be of equal importance.