Abstract. Previous multi-model intercomparisons have shown that chemistry–climate
models exhibit significant biases in tropospheric ozone compared with
observations. We investigate annual-mean tropospheric column ozone in 15
models participating in the SPARC–IGAC (Stratosphere–troposphere Processes
And their Role in Climate–International Global Atmospheric Chemistry)
Chemistry-Climate Model Initiative (CCMI). These models exhibit a positive
bias, on average, of up to 40 %–50 % in the Northern Hemisphere compared with
observations derived from the Ozone Monitoring Instrument and Microwave Limb
Sounder (OMI/MLS), and a negative bias of up to ∼30 % in the Southern
Hemisphere. SOCOLv3.0 (version 3 of the Solar-Climate Ozone Links CCM), which
participated in CCMI, simulates global-mean tropospheric ozone columns of
40.2 DU – approximately 33 % larger than the CCMI multi-model mean. Here we
introduce an updated version of SOCOLv3.0, “SOCOLv3.1”, which includes an
improved treatment of ozone sink processes, and results in a reduction in the
tropospheric column ozone bias of up to 8 DU, mostly due to the inclusion of
N2O5 hydrolysis on tropospheric aerosols. As a result of these
developments, tropospheric column ozone amounts simulated by SOCOLv3.1 are
comparable with several other CCMI models. We apply Gaussian process
emulation and sensitivity analysis to understand the remaining ozone bias in
SOCOLv3.1. This shows that ozone precursors (nitrogen oxides
(NOx), carbon monoxide, methane and other volatile organic
compounds, VOCs) are responsible for more than 90 % of the variance in tropospheric
ozone. However, it may not be the emissions inventories themselves that
result in the bias, but how the emissions are handled in SOCOLv3.1, and we
discuss this in the wider context of the other CCMI models. Given that the
emissions data set to be used for phase 6 of the Coupled Model
Intercomparison Project includes approximately 20 % more NOx
than the data set used for CCMI, further work is urgently needed to address
the challenges of simulating sub-grid processes of importance to tropospheric
ozone in the current generation of chemistry–climate models.