Dissecting cirrus clouds: navigating effects of turbulence on homogeneous ice formation

Abstract Turbulent air motions determine the local environment in which cloud ice crystals form. Homogeneous freezing of aqueous solution droplets is the most fundamental pathway to nucleate ice crystals in cirrus. Lack of knowledge about the role of turbulence in cirrus ice formation limits our understanding of how uncertainties in small-scale cloud processes affect the climatological radiative effect of cirrus. Here we shed first light on how turbulent fluctuations in temperature and supersaturation interact with probabilistic homogeneous freezing. We show that spatial model resolution substantially below 1–10 m is needed to properly simulate homogeneous freezing events. Importantly, microscale turbulence generates large variability in nucleated ice crystal number concentrations. Previous research ascribed this variability to mesoscale dynamical forcing due to gravity waves alone. The turbulence-generated microphysical variability has macrophysical implications. The wide range of predicted cloud radiative heating anomalies in anvil cirrus due to turbulence-ice nucleation interactions, comparable to typical mean values, is potentially large enough to affect the response of tropical cirrus cloud systems to global warming. Our results have ramifications for the multiscale modeling of cirrus clouds and the interpretation of in situ measurements.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2025-04-05
DOI
https://doi.org/10.1038/s41612-025-01024-w
Citations
1
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
1.11

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article

Dissecting cirrus clouds: navigating effects of turbulence on homogeneous ice formation

Aurélien Podglajen, Rachel Atlas, Albert Hertzog, B. Kärcher et al.
1 citations
npj Climate and Atmospheric Science
Atmospheric aerosols and clouds
1.11
article

Dissecting cirrus clouds: navigating effects of turbulence on homogeneous ice formation

Aurélien Podglajen, Rachel Atlas, Albert Hertzog, B. Kärcher, Adam B. Sokol, Wojciech W. Grabowski, Riwal Plougonven, E. J. Jensen, Blaž Gasparini, Fabian Hoffmann, Milena Corcos, Hugh Morrison, Kamal Kant Chandrakhar
article en
1 citations

Abstract

Abstract Turbulent air motions determine the local environment in which cloud ice crystals form. Homogeneous freezing of aqueous solution droplets is the most fundamental pathway to nucleate ice crystals in cirrus. Lack of knowledge about the role of turbulence in cirrus ice formation limits our understanding of how uncertainties in small-scale cloud processes affect the climatological radiative effect of cirrus. Here we shed first light on how turbulent fluctuations in temperature and supersaturation interact with probabilistic homogeneous freezing. We show that spatial model resolution substantially below 1–10 m is needed to properly simulate homogeneous freezing events. Importantly, microscale turbulence generates large variability in nucleated ice crystal number concentrations. Previous research ascribed this variability to mesoscale dynamical forcing due to gravity waves alone. The turbulence-generated microphysical variability has macrophysical implications. The wide range of predicted cloud radiative heating anomalies in anvil cirrus due to turbulence-ice nucleation interactions, comparable to typical mean values, is potentially large enough to affect the response of tropical cirrus cloud systems to global warming. Our results have ramifications for the multiscale modeling of cirrus clouds and the interpretation of in situ measurements.

npj Climate and Atmospheric ScienceVol. 8(1)
NSF National Center for Atmospheric Research (US), Centre National de la Recherche Scientifique (FR), University of Vienna (AT), National Oceanic and Atmospheric Administration (US), Princeton University (US), Université Paris Sciences et Lettres (FR), Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR) (DE), École Normale Supérieure - PSL (FR), Sorbonne Université (FR), Laboratoire de Météorologie Dynamique (FR), Institut Pierre-Simon Laplace (FR), NOAA Chemical Sciences Laboratory (US), Northwest Research Associates (US), Ludwig-Maximilians-Universität München (DE)
National Science Foundation, U.S. Department of Commerce, European Commission, Deutsche Forschungsgemeinschaft, Agence Nationale de la Recherche, Deutsches Zentrum für Luft- und Raumfahrt, National Oceanic and Atmospheric Administration
Openalex Percentile: Top 26%
Atmospheric aerosols and clouds
1.11
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