Preprints
https://doi.org/10.5194/egusphere-2025-6077
https://doi.org/10.5194/egusphere-2025-6077
11 Mar 2026
 | 11 Mar 2026
Status: this preprint is open for discussion and under review for Geoscientific Model Development (GMD).

Assimilation of ground based lidar and ceilometer observations of aerosols from the European E-Profile network into ECMWF's Integrated Forecasting System (IFS-COMPO, CY49R1)

Michael Kahnert, Melanie Ades, Mickaël Bacles, Johannes Flemming, Vincent Guidard, Alexander Haefele, Robin J. Hogan, Samuel Rémy, and Eric Sauvageat

Abstract. The Integrated Forecasting System with its extension for atmospheric composition (IFS-COMPO) provides global forecasts of atmospheric trace gases and aerosols for the Copernicus Atmosphere Monitoring Service (CAMS). The present system constrains aerosol concentrations by assimilating aerosol optical depth (AOD) from different satellites. Here, we explore the possibility of assimilating, in addition, ground-based lidar and ceilometer observations from the European E-Profile network. The system performance is evaluated by comparison to non-assimilated E-Profile stations, AOD observations from Aeronet, and aerosol surface concentrations from AirBase. Assimilation of E-Profile data significantly reduces biases and root mean square errors (RMSE) of model-equivalent vertical profiles of the attenuated backscatter coefficient. Without assimilation of E-Profile, surface concentrations of particles smaller than 2.5 μm (PM2.5) are frequently overestimated during summer, while corresponding concentrations of particles smaller than 10 μm (PM10) tend to be underestimated. Assimilation of E-Profile can reduce the RMSE of PM2.5 by up to 50 % and of PM10 by up to 10 %. Since the present analysis system uses the total aerosol mass mixing ratio as control variable, it cannot simultaneously reduce the positive PM2.5 bias and the negative PM10 bias. It typically reduces the PM2.5 bias at the expense of PM10, since fine particles make the dominant contribution to the optical cross sections per mass. Tests of different assimilation-system configurations reveal that the best overall performance is obtained by treating optical properties of dust with a spheroid model, suppressing vertical correlations in the background error covariances, and applying a relatively aggressive cloud mask.

Competing interests: Co-author Samuel Rémy is a member of the editorial board of Geosci. Mod. Dev.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Michael Kahnert, Melanie Ades, Mickaël Bacles, Johannes Flemming, Vincent Guidard, Alexander Haefele, Robin J. Hogan, Samuel Rémy, and Eric Sauvageat

Status: open (until 06 May 2026)

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Michael Kahnert, Melanie Ades, Mickaël Bacles, Johannes Flemming, Vincent Guidard, Alexander Haefele, Robin J. Hogan, Samuel Rémy, and Eric Sauvageat
Michael Kahnert, Melanie Ades, Mickaël Bacles, Johannes Flemming, Vincent Guidard, Alexander Haefele, Robin J. Hogan, Samuel Rémy, and Eric Sauvageat

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Short summary
The Copernicus Atmosphere Monitoring Service (CAMS) provides quality-controlled information related to air quality and health. We explore the possibility to constrain the CAMS global forecasting model by use of ground-based observations of laser light backscattered by particulate matter. We find that the vertical distribution of particulate matter can be predicted more faithfully with this approach, which can have implications for air quality forecasts provided by CAMS to end users.
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