Ice fog and supersaturation observed at cirrus temperatures at Dome C, Antarctic Plateau ...

<!--!introduction!--> As the near-surface atmosphere over the Antarctic Plateau is cold and pristine, its physico-chemical conditions resemble to a certain extent those of the high troposphere where cirrus clouds form. In this study, we carry out an observational analysis of two shallow fog cl...

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Bibliographic Details
Main Authors: Vignon, Étienne, Raillard, Lea, Genthon, Christophe, Del Guasta, Massimo, Heymsfield, Andrew, Madeleine, Jean-Baptiste, Berne, Alexis
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
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Online Access:https://dx.doi.org/10.57757/iugg23-2382
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018393
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Summary:<!--!introduction!--> As the near-surface atmosphere over the Antarctic Plateau is cold and pristine, its physico-chemical conditions resemble to a certain extent those of the high troposphere where cirrus clouds form. In this study, we carry out an observational analysis of two shallow fog clouds forming in situ at cirrus temperatures – that is, temperatures lower than 235 K – at Dome C, Antarctic Plateau. The combination of lidar profiles with temperature and humidity measurements from advanced thermo-hygrometers along a 45 m mast makes it possible to characterise the formation and development of the fog. High supersaturations with respect to ice are observed before the initiation of fog, and the values attained suggest that the nucleation process at play is the homogeneous freezing of solution aerosol droplets. Once nucleation occurs, the relative humidity decreases down to subsaturated values with respect to ice in a few hours, owing to vapour deposition onto ice crystals and turbulent mixing. The ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...