Preprints
https://doi.org/10.5194/egusphere-2026-2958
https://doi.org/10.5194/egusphere-2026-2958
22 Jul 2026
 | 22 Jul 2026
Status: this preprint is open for discussion and under review for Atmospheric Measurement Techniques (AMT).

Overhaul of the stratospheric lidar at Dumont d’Urville, Antarctica: three-wavelength setup, processing and observations

Florent Tencé, Julien Jumelet, Rafik Hassen-Khodja, Sophie Bounissou, Jean-François Mariscal, and Ismaël Charlet

Abstract. The stratospheric cloud and aerosol lidar instrument Liraan (LIdar pour la Recherche Antarctique Aérosol et Nuages) has been operated at the French Antarctic station Dumont d'Urville since 1989. Following a major upgrade conducted between 2022 and 2024, this paper presents the instrument configuration and its scientific capabilities. Liraan now enables the retrieval of backscatter coefficients at 355 nm, 532 nm and 1064 nm and depolarization ratios at 355 nm and 532 nm. The new configuration is described in detail, along with an improved data inversion algorithm, which is further used as input to a dedicated microphysical retrieval methodology. A unified 532 nm lidar time series spanning 19912025 at Dumont d'Urville is also presented for the first time. Finally, 2025 multispectral lidar measurements are used in a case study of volcanic aerosol size distribution retrieval.

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Florent Tencé, Julien Jumelet, Rafik Hassen-Khodja, Sophie Bounissou, Jean-François Mariscal, and Ismaël Charlet

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Florent Tencé, Julien Jumelet, Rafik Hassen-Khodja, Sophie Bounissou, Jean-François Mariscal, and Ismaël Charlet
Florent Tencé, Julien Jumelet, Rafik Hassen-Khodja, Sophie Bounissou, Jean-François Mariscal, and Ismaël Charlet

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Short summary
The stratospheric lidar at the French Antarctic station Dumont d’Urville has been upgraded to simultaneously operate at 355, 532 and 1064 nm. We present the new setup and an updated inversion algorithm used to produce the first 34-year record of Antarctic lidar observations. A 2025 case study uses these measurements to estimate the microphysical properties of volcanic aerosols. This capability is critical in the context of stratospheric perturbations caused by wildfires and volcanic eruptions.
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