Preprints
https://doi.org/10.5194/egusphere-2025-4298
https://doi.org/10.5194/egusphere-2025-4298
06 Nov 2025
 | 06 Nov 2025
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

A framework to holistically investigate processes controlling the aerosol lifecycle using explainable AI techniques

Eliza K. Duncan, Jonathan E. Fieldsend, Alistair Sellar, Emmanuele Tovazzi, Paul Kim, James M. Haywood, and Daniel G. Partridge

Abstract. General circulation models (GCMs) face significant uncertainties in estimating Earth's radiative budget due to aerosol-cloud interactions (ACI). To improve the representation of ACI in GCMs it is crucial to constrain processes controlling the aerosol lifecycle and the resulting size distribution. This is challenging due to the complexity and number of competing atmospheric processes that interact over large spatial and temporal scales which require untangling to elucidate dominant processes controlling aerosol properties. This study aims to (a) develop a generic explainable AI framework from air-mass history to build an accurate representation of processes controlling aerosol properties, from this, (b) identify key relationships between aerosol processes and their impacts on observed aerosol number concentrations, and (c) provide robust process-based observational constraints to aid in the isolation of GCM structural uncertainties. This is achieved by developing XGBoost regression models to simulate Aitken and accumulation mode number concentrations for receptor surface stations and application of TreeSHAP to identify key processes from explanatory variables describing meteorological and aerosol processes collocated to Lagrangian air-mass trajectories. The fidelity of this framework is demonstrated for the Antarctic station Trollhaugen, situated in a pristine region in which GCMs exhibit significant biases. Aerosol number concentrations at Trollhaugen were shown to be dominated by marine sources as well as transport from the free troposphere. The contribution from aloft dominates aerosol burden of the Aitken mode in the transitions between summer and winter, in contrast to a larger contribution in the summer from local marine sources from transport in the boundary layer.

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Eliza K. Duncan, Jonathan E. Fieldsend, Alistair Sellar, Emmanuele Tovazzi, Paul Kim, James M. Haywood, and Daniel G. Partridge

Status: open (until 18 Dec 2025)

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Eliza K. Duncan, Jonathan E. Fieldsend, Alistair Sellar, Emmanuele Tovazzi, Paul Kim, James M. Haywood, and Daniel G. Partridge
Eliza K. Duncan, Jonathan E. Fieldsend, Alistair Sellar, Emmanuele Tovazzi, Paul Kim, James M. Haywood, and Daniel G. Partridge
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Short summary
Atmospheric aerosol particles are a major confounding factor in accurately representing climate change. We build a novel generic framework to untangle the role of complex processes focusing on a remote site in Antarctica as a case study in near-pristine conditions. Our machine-learning model predicts aerosol concentrations from an airmass history, considering the meteorology and potential sources and removal processes, enabling improved representation in climate models.
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