Articles | Volume 20, issue 7
https://doi.org/10.5194/acp-20-4167-2020
https://doi.org/10.5194/acp-20-4167-2020
Research article
 | Highlight paper
 | 
07 Apr 2020
Research article | Highlight paper |  | 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, Massimo Del Guasta, Eric Bazile, Niramson Azouz, Angelo Lupi, Pierre Durand, Jean-Luc Attié, Dana Veron, Vincent Guidard, and Paolo Grigioni

Viewed

Total article views: 4,116 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,286 755 75 4,116 180 94 87
  • HTML: 3,286
  • PDF: 755
  • XML: 75
  • Total: 4,116
  • Supplement: 180
  • BibTeX: 94
  • EndNote: 87
Views and downloads (calculated since 28 Aug 2019)
Cumulative views and downloads (calculated since 28 Aug 2019)

Viewed (geographical distribution)

Total article views: 4,116 (including HTML, PDF, and XML) Thereof 3,905 with geography defined and 211 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 01 Nov 2024
Download
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.
Altmetrics
Final-revised paper
Preprint