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

Authors :
Johnson, Jill S.
Regayre, Leighton A.
Yoshioka, Masaru
Pringle, Kirsty J.
Turnock, Steven T.
Browse, Jo
Sexton, David M. H.
Rostron, John W.
Schutgens, Nick A. J.
Partridge, Daniel G.
Dantong Liu
Allan, James D.
Hugh Coe
Ding, Aijun
Cohen, David D.
Atanacio, Armand
Vakkari, Ville
Asmi, Eija
Carslaw, Ken S.
Source :
Atmospheric Chemistry & Physics Discussions; 2019, p1-51, 51p
Publication Year :
2019

Abstract

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 HadGEM3-UKCA climate model that sample 26 sources of uncertainty, together with over 9000 monthly aggregated grid-box measurements of aerosol optical depth, PM<subscript>2.5</subscript>, particle number concentrations, sulphate 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 SO<subscript>2</subscript> emissions, residential emissions, sea spray emissions, dry deposition rates of SO<subscript>2</subscript> 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, the ± 1σ (standard deviation) range of global annual mean direct radiative forcing, RF<subscript>ari</subscript>, is reduced by 33 % to -0.14 to -0.26 W m<superscript>-2</superscript>, and the 95 % credible interval (CI) is reduced by 34 % to -0.1 to -0.32 W m<superscript>-2</superscript>. For the global annual mean aerosol-cloud radiative forcing, RF<subscript>aci</subscript>, the ± 1σ range is reduced by 7 % to -1.66 to -2.48 W m<superscript>-2</superscript>, and the 95 % CI by 6 % to -1.28 to -2.88 W m<superscript>-2</superscript>. The tightness of the constraint is limited by parameter cancellation effects (model equifinality) as well as the large and poorly defined <q>representativeness error</q> 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, constraints using either sulphate or PM<subscript>2.5</subscript> measurements individually result in RF<subscript>ari</subscript> ± 1σ ranges that only just overlap, which shows that emergent constraints based on one measurement type may be over-confident. [ABSTRACT FROM AUTHOR]

Details

Language :
Polish
ISSN :
16807367
Database :
Complementary Index
Journal :
Atmospheric Chemistry & Physics Discussions
Publication Type :
Academic Journal
Accession number :
140046238
Full Text :
https://doi.org/10.5194/acp-2019-834