Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery

Abstract The 15 January 2022 eruption of the Hunga volcano generated a Lamb wave, a global atmospheric pressure perturbation which propagates purely horizontally at the speed of sound. Far‐field observations of the daytime passage of the Lamb wave by the Geostationary Operational Environmental Satellite‐R (GOES‐R) series, revealed unexpected, synchronized variations in the solar reflectance of low‐level liquid clouds, the most prominent of which is a transient darkening accompanying the overpressure peak. We hypothesize that this darkening is mostly caused by the rapid thermodynamic adjustment of the cloudy environment to the slight, but spatially coherent, warming introduced by the pressure pulse. The corresponding reduction in relative humidity leads to the shrinkage and evaporation of small cloud droplets and hygroscopic particles in the halo region, which, in turn, temporarily reduces the optical thickness of the cloudy column.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-06-21
DOI
https://doi.org/10.1029/2025gl115935
Citations
1
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
1.11

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article

Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery

Mirjana Sakradžija, M. Liu, Stefan A. Buehler, David K. Adams et al.
1 citations
Geophysical Research Letters
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article

Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery

Mirjana Sakradžija, M. Liu, Stefan A. Buehler, David K. Adams, Ignacio Sepúlveda, Ákos Horváth
article en
1 citations

Abstract

Abstract The 15 January 2022 eruption of the Hunga volcano generated a Lamb wave, a global atmospheric pressure perturbation which propagates purely horizontally at the speed of sound. Far‐field observations of the daytime passage of the Lamb wave by the Geostationary Operational Environmental Satellite‐R (GOES‐R) series, revealed unexpected, synchronized variations in the solar reflectance of low‐level liquid clouds, the most prominent of which is a transient darkening accompanying the overpressure peak. We hypothesize that this darkening is mostly caused by the rapid thermodynamic adjustment of the cloudy environment to the slight, but spatially coherent, warming introduced by the pressure pulse. The corresponding reduction in relative humidity leads to the shrinkage and evaporation of small cloud droplets and hygroscopic particles in the halo region, which, in turn, temporarily reduces the optical thickness of the cloudy column.

Geophysical Research LettersVol. 52(12)
Universität Hamburg (DE), Chengdu University of Information Technology (CN), San Diego State University (US), Ludwig-Maximilians-Universität München (DE), Universidad Nacional Autónoma de México (MX)
Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 23%
Atmospheric aerosols and clouds
1.11
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