Articles | Volume 20, issue 7
https://doi.org/10.5194/acp-20-4167-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-4167-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
07 Apr 2020
Research article | Highlight paper |
| 07 Apr 2020
| 07 Apr 2020
Supercooled liquid water cloud observed, analysed, and modelled at the top of the planetary boundary layer above Dome C, Antarctica
CNRM, Université de Toulouse, Météo-France, CNRS,
Toulouse, France
Massimo Del Guasta
INO-CNR, Sesto Fiorentino, Italy
Eric Bazile
CNRM, Université de Toulouse, Météo-France, CNRS,
Toulouse, France
Niramson Azouz
CNRM, Université de Toulouse, Météo-France, CNRS,
Toulouse, France
Angelo Lupi
ISAC-CNR, Bologna, Italy
Pierre Durand
Laboratoire d'Aérologie, Université de Toulouse, CNRS, UPS,
Toulouse, France
Jean-Luc Attié
Laboratoire d'Aérologie, Université de Toulouse, CNRS, UPS,
Toulouse, France
Dana Veron
University of Delaware, Newark, USA
Vincent Guidard
CNRM, Université de Toulouse, Météo-France, CNRS,
Toulouse, France
Paolo Grigioni
ENEA, Roma, Italy
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Cited
15 citations as recorded by crossref.
- In situ observations of supercooled liquid water clouds over Dome C, Antarctica, by balloon-borne sondes P. Ricaud et al. 10.5194/amt-17-5071-2024
- Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses P. Ricaud et al. 10.3390/atmos11080836
- Comprehensive Evaluation and Comparison of AIRS, VASS, and VIRR Water Vapor Products Over Antarctica R. Fan et al. 10.1029/2023JD039221
- Challenging and Improving the Simulation of Mid‐Level Mixed‐Phase Clouds Over the High‐Latitude Southern Ocean É. Vignon et al. 10.1029/2020JD033490
- Ice and mixed-phase cloud statistics on the Antarctic Plateau W. Cossich et al. 10.5194/acp-21-13811-2021
- Ice fog observed at cirrus temperatures at Dome C, Antarctic Plateau É. Vignon et al. 10.5194/acp-22-12857-2022
- Supercooled liquid water clouds observed over Dome C, Antarctica: temperature sensitivity and cloud radiative forcing P. Ricaud et al. 10.5194/acp-24-613-2024
- Satellite Microwave Radiometric Measurements of Extreme Temperature Rise in East Antarctica in March 2022 L. Mitnik et al. 10.1134/S0010952523700612
- Water vapor in cold and clean atmosphere: a 3-year data set in the boundary layer of Dome C, East Antarctic Plateau C. Genthon et al. 10.5194/essd-14-1571-2022
- Refractive Index of Supercooled Water Down to 230.3 K in the Wavelength Range between 534 and 675 nm C. Goy et al. 10.1021/acs.jpclett.2c02803
- Increasing Antarctic Ice Mass to Help Offset Sea Level Rise E. Larson et al. 10.3390/atmos14101564
- Detection of supercooled liquid water containing clouds with ceilometers: development and evaluation of deterministic and data-driven retrievals A. Guyot et al. 10.5194/amt-15-3663-2022
- Assessing the simulation of snowfall at Dumont d'Urville, Antarctica, during the YOPP‐SH special observing campaign M. Roussel et al. 10.1002/qj.4463
- In Situ VTOL Drone-Borne Observations of Temperature and Relative Humidity over Dome C, Antarctica P. Ricaud et al. 10.3390/drones7080532
- 10 years of temperature and wind observation on a 45 m tower at Dome C, East Antarctic plateau C. Genthon et al. 10.5194/essd-13-5731-2021
15 citations as recorded by crossref.
- In situ observations of supercooled liquid water clouds over Dome C, Antarctica, by balloon-borne sondes P. Ricaud et al. 10.5194/amt-17-5071-2024
- Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses P. Ricaud et al. 10.3390/atmos11080836
- Comprehensive Evaluation and Comparison of AIRS, VASS, and VIRR Water Vapor Products Over Antarctica R. Fan et al. 10.1029/2023JD039221
- Challenging and Improving the Simulation of Mid‐Level Mixed‐Phase Clouds Over the High‐Latitude Southern Ocean É. Vignon et al. 10.1029/2020JD033490
- Ice and mixed-phase cloud statistics on the Antarctic Plateau W. Cossich et al. 10.5194/acp-21-13811-2021
- Ice fog observed at cirrus temperatures at Dome C, Antarctic Plateau É. Vignon et al. 10.5194/acp-22-12857-2022
- Supercooled liquid water clouds observed over Dome C, Antarctica: temperature sensitivity and cloud radiative forcing P. Ricaud et al. 10.5194/acp-24-613-2024
- Satellite Microwave Radiometric Measurements of Extreme Temperature Rise in East Antarctica in March 2022 L. Mitnik et al. 10.1134/S0010952523700612
- Water vapor in cold and clean atmosphere: a 3-year data set in the boundary layer of Dome C, East Antarctic Plateau C. Genthon et al. 10.5194/essd-14-1571-2022
- Refractive Index of Supercooled Water Down to 230.3 K in the Wavelength Range between 534 and 675 nm C. Goy et al. 10.1021/acs.jpclett.2c02803
- Increasing Antarctic Ice Mass to Help Offset Sea Level Rise E. Larson et al. 10.3390/atmos14101564
- Detection of supercooled liquid water containing clouds with ceilometers: development and evaluation of deterministic and data-driven retrievals A. Guyot et al. 10.5194/amt-15-3663-2022
- Assessing the simulation of snowfall at Dumont d'Urville, Antarctica, during the YOPP‐SH special observing campaign M. Roussel et al. 10.1002/qj.4463
- In Situ VTOL Drone-Borne Observations of Temperature and Relative Humidity over Dome C, Antarctica P. Ricaud et al. 10.3390/drones7080532
- 10 years of temperature and wind observation on a 45 m tower at Dome C, East Antarctic plateau C. Genthon et al. 10.5194/essd-13-5731-2021
Latest update: 20 Nov 2024
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.
Thin (~ 100 m) supercooled liquid water (SLW, water staying in liquid phase below 0 °C)...
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