Abstract

Abstract. Atmospheric chemistry transport models (ACTMs) are widely used to underpin policy decisions associated with the impact of potential changes in emissions on future pollutant concentrations and deposition. It is therefore essential to have a quantitative understanding of the uncertainty in model output arising from uncertainties in the input pollutant emissions. ACTMs incorporate complex and non-linear descriptions of chemical and physical processes which means that interactions and non-linearities in input–output relationships may not be revealed through the local one-at-a-time sensitivity analysis typically used. The aim of this work is to demonstrate a global sensitivity and uncertainty analysis approach for an ACTM, using as an example the FRAME model, which is extensively employed in the UK to generate source–receptor matrices for the UK Integrated Assessment Model and to estimate critical load exceedances. An optimised Latin hypercube sampling design was used to construct model runs within ±40 % variation range for the UK emissions of SO2, NOx, and NH3, from which regression coefficients for each input–output combination and each model grid ( > 10 000 across the UK) were calculated. Surface concentrations of SO2, NOx, and NH3 (and of deposition of S and N) were found to be predominantly sensitive to the emissions of the respective pollutant, while sensitivities of secondary species such as HNO3 and particulate SO42−, NO3−, and NH4+ to pollutant emissions were more complex and geographically variable. The uncertainties in model output variables were propagated from the uncertainty ranges reported by the UK National Atmospheric Emissions Inventory for the emissions of SO2, NOx, and NH3 (±4, ±10, and ±20 % respectively). The uncertainties in the surface concentrations of NH3 and NOx and the depositions of NHx and NOy were dominated by the uncertainties in emissions of NH3, and NOx respectively, whilst concentrations of SO2 and deposition of SOy were affected by the uncertainties in both SO2 and NH3 emissions. Likewise, the relative uncertainties in the modelled surface concentrations of each of the secondary pollutant variables (NH4+, NO3−, SO42−, and HNO3) were due to uncertainties in at least two input variables. In all cases the spatial distribution of relative uncertainty was found to be geographically heterogeneous. The global methods used here can be applied to conduct sensitivity and uncertainty analyses of other ACTMs.

Highlights

  • Atmospheric chemistry transport models (ACTMs) provide scientific support for policy development

  • Regression coefficients (RCs) show the sensitivity of each model output variable to the three input emissions variables (SO2, nitrogen oxides (NOx), and NH3) and can be interpreted as a magnitude of the response of an output to the unit change in a particular input when all other inputs are allowed to vary

  • The magnitude of the RCs provides useful information about the effect of the change in a particular input on a model output and allows input sensitivity ranking to be determined because all inputs were assigned the same range of variation (±40 %)

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Summary

Introduction

Atmospheric chemistry transport models (ACTMs) provide scientific support for policy development. It is important to have a quantitative understanding of the levels of uncertainty associated with model outputs (AQEG, 2015; Frost et al, 2013; Rypdal and Winiwarter, 2001). Uncertainty analysis is applied to quantify the propagation of uncertainties of single or multiple inputs through to a model output, whilst sensitivity analysis is used to investigate input–output relationships and to apportion the variation in model output to the different inputs. K. Aleksankina et al.: Global sensitivity and uncertainty analysis of ACTM the complexity of ACTMs, the relationship between model inputs and outputs is not analytically tractable, so both quantities must be estimated by sampling model inputs according to an experimental design and undertaking multiple model simulations (Dean et al, 2015; Norton, 2015; Saltelli et al, 2000; Saltelli and Annoni, 2010)

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