Robust observational constraint of uncertain aerosol processes and emissions in a climate model and the effect on aerosol radiative forcing

Jill S. Johnson, Leighton A. Regayre, Masaru Yoshioka, Kirsty J. Pringle, Steven T. Turnock, Jo Browse, David M.H. Sexton, John W. Rostron, Nick A.J. Schutgens, Daniel G. Partridge, Dantong Liu, James D. Allan, Hugh Coe, Aijun DIng, David D. Cohen, Armand Atanacio, Ville Vakkari, Eija Asmi, Ken S. Carslaw

Research output: Contribution to journalArticlepeer-review


The effect of observational constraint on the ranges of uncertain physical and chemical process parameters was explored in a global aerosol-climate model. The study uses 1 million variants of the Hadley Centre General Environment Model version 3 (HadGEM3) that sample 26 sources of uncertainty, together with over 9000 monthly aggregated grid-box measurements of aerosol optical depth, PM2:5, particle number concentrations, sulfate and organic mass concentrations. Despite many compensating effects in the model, the procedure constrains the probability distributions of parameters related to secondary organic aerosol, anthropogenic SO2 emissions, residential emissions, sea spray emissions, dry deposition rates of SO2 and aerosols, new particle formation, cloud droplet pH and the diameter of primary combustion particles. Observational constraint rules out nearly 98% of the model variants. On constraint, the1 (standard deviation) range of global annual mean direct radiative forcing (RFari) is reduced by 33% to ±0:14 to ±0:26Wm±2, and the 95% credible interval (CI) is reduced by 34% to ±0:1 to ±0:32Wm±2. For the global annual mean aerosol-cloud radiative forcing, RFaci, the1 range is reduced by 7% to ±1:66 to ±2:48Wm±2, and the 95% CI by 6% to ±1:28 to ±2:88Wm±2. The tightness of the constraint is limited by parameter cancellation effects (model equifinality) as well as the large and poorly defined "representativeness error" associated with comparing point measurements with a global model. The constraint could also be narrowed if model structural errors that prevent simultaneous agreement with different measurement types in multiple locations and seasons could be improved. For example, con straints using either sulfate or PM2:5 measurements individually result in RFari1 ranges that only just overlap, which shows that emergent constraints based on one measurement type may be overconfident.

Original languageEnglish
Pages (from-to)9491-9524
Number of pages34
JournalAtmospheric Chemistry and Physics
Issue number15
Publication statusPublished - 13 Aug 2020


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