Preprints
https://doi.org/10.5194/egusphere-2025-5905
https://doi.org/10.5194/egusphere-2025-5905
05 Jan 2026
 | 05 Jan 2026
Status: this preprint is open for discussion and under review for Atmospheric Measurement Techniques (AMT).

Measuring cloud optical depth with a balloonborne microlidar operated from the stratosphere

François Ravetta, Thomas Lesigne, Vincent Mariage, and Jacques Pelon

Abstract. The Balloonborne Cloud Observing micrOLidar (BeCOOL) has been developed to be operated onboard a stratospheric balloon in order  to monitor the atmosphere below 20 km, more particularly thin ice clouds. This lidar system was designed to maintain a high level of performance while keeping its mass below 6 kg and limiting its power consumption to 4 W on average. Several balloons embarking BeCOOL instruments have been launched from the Tropics (Seychelles Islands, 4.68 S +55.45 E)  during the STRATEOLE-2 campaign organized by the French Space Agency (Centre National d'Etudes Spatiales, CNES) in autumn and winter 20212022. The microlidar system, its operational performances, and the data processing to estimate optical properties are described. BeCOOL is able to measure optical depth of upper level thin ice clouds down to 2 × 10−5. It is possible to constrain the lidar ratio when the cloud optical depth is larger than 3 × 10−2. In this case, the optical depth relative uncertainty is less than 10 %.

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François Ravetta, Thomas Lesigne, Vincent Mariage, and Jacques Pelon

Status: open (until 10 Feb 2026)

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  • RC1: 'Comment on egusphere-2025-5905', Robin Wing, 06 Jan 2026 reply
François Ravetta, Thomas Lesigne, Vincent Mariage, and Jacques Pelon
François Ravetta, Thomas Lesigne, Vincent Mariage, and Jacques Pelon

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Short summary
The Balloonborne Cloud Observing micrOLidar (BeCOOL) is an airborne profiler designed to monitor cirrus clouds from the stratosphere. It weights less than 6 kg and requires on average less than 4 W to work automatically onboard a gondola attached below a stratospheric balloon. Given its sensitivity, it can be used to calibrate or validate satellite observations, or to study the life cycle of cirrus clouds.
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