Articles | Volume 17, issue 17
https://doi.org/10.5194/amt-17-5071-2024
https://doi.org/10.5194/amt-17-5071-2024
Research article
 | 
03 Sep 2024
Research article |  | 03 Sep 2024

In situ observations of supercooled liquid water clouds over Dome C, Antarctica, by balloon-borne sondes

Philippe Ricaud, Pierre Durand, Paolo Grigioni, Massimo Del Guasta, Giuseppe Camporeale, Axel Roy, Jean-Luc Attié, and John Bognar

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Cited articles

Bain, M. and Gayet, J. F.: Aircraft measurements of icing in supercooled and water droplet/ice crystal clouds, J. Appl. Meteorol., 21, 631–641, https://www.jstor.org/stable/26180452 (last access: 27 August 2024), 1982. 
Bromwich, D. H., Otieno, F. O., Hines, K. M., Manning, K. W., and Shilo, E.: Comprehensive evaluation of polar weather research and forecasting model performance in the Antarctic, J. Geophys. Res.-Atmos., 118, 274–292, 2013. 
Chubb, T. H., Jensen, J. B., Siems, S. T., and Manton, M. J.: In situ observations of supercooled liquid clouds over the Southern Ocean during the HIAPER pole-to-pole observation campaigns, Geophys. Res. Lett., 40, 5280–5285, 2013. 
Cossich, W., Maestri, T., Magurno, D., Martinazzo, M., Di Natale, G., Palchetti, L., Bianchini, G., and Del Guasta, M.: Ice and mixed-phase cloud statistics on the Antarctic Plateau, Atmos. Chem. Phys., 21, 13811–13833, https://doi.org/10.5194/acp-21-13811-2021, 2021. 
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Short summary
Clouds in Antarctica are key elements affecting climate evolution. Some clouds are composed of supercooled liquid water (SLW; water held in liquid form below 0 °C) and are difficult to forecast by models. We performed in situ observations of SLW clouds at Concordia Station using SLW sondes attached to meteorological balloons in summer 2021–2022. The SLW clouds were observed in a saturated layer at the top of the planetary boundary layer in agreement with ground-based lidar observations.
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