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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Thin (~ 100 m) supercooled liquid water (SLW, water staying in liquid phase below 0 °C) clouds have been detected, analysed, and modelled over the Dome C (Concordia, Antarctica) station during the austral summer 2018–2019 using observations and meteorological analyses. The SLW clouds were observed at the top of the planetary boundary layer and the SLW content was always strongly underestimated by the model indicating an incorrect simulation of the surface energy budget of the Antarctic Plateau.
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ACP | Articles | Volume 20, issue 7
Atmos. Chem. Phys., 20, 4167–4191, 2020
https://doi.org/10.5194/acp-20-4167-2020
Atmos. Chem. Phys., 20, 4167–4191, 2020
https://doi.org/10.5194/acp-20-4167-2020

Research article 07 Apr 2020

Research article | 07 Apr 2020

Supercooled liquid water cloud observed, analysed, and modelled at the top of the planetary boundary layer above Dome C, Antarctica

Philippe Ricaud et al.

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Latest update: 24 Jan 2021
Publications Copernicus
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Short summary
Thin (~ 100 m) supercooled liquid water (SLW, water staying in liquid phase below 0 °C) clouds have been detected, analysed, and modelled over the Dome C (Concordia, Antarctica) station during the austral summer 2018–2019 using observations and meteorological analyses. The SLW clouds were observed at the top of the planetary boundary layer and the SLW content was always strongly underestimated by the model indicating an incorrect simulation of the surface energy budget of the Antarctic Plateau.
Citation
Altmetrics
Final-revised paper
Preprint