Articles | Volume 17, issue 8
https://doi.org/10.5194/acp-17-5221-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-5221-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Apr 2017
Research article |
| 21 Apr 2017
Genesis of diamond dust, ice fog and thick cloud episodes observed and modelled above Dome C, Antarctica
Météo-France/CNRM, CNRS UMR 3589, 42 avenue Gaspard Coriolis,
31057 Toulouse, France
Eric Bazile
Météo-France/CNRM, CNRS UMR 3589, 42 avenue Gaspard Coriolis,
31057 Toulouse, France
Massimo del Guasta
INO-CNR, Via Madonna del Piano 10, 50019, Sesto Fiorentino, Italy
Christian Lanconelli
Institute of Atmospheric Sciences and Climate (ISAC), Consiglio
Nazionale delle Ricerche, via Gobetti 101, 40129 Bologna, Italy
now at: Joint Research Center, Institute for Environment and
Sustainability (IES), Land Resource Management Unit (H05), via Fermi, 21027
Ispra (VA), Italy
Paolo Grigioni
ENEA, Lungotevere Thaon di Revel, 76-00196 Roma, Italy
Achraf Mahjoub
Météo-France/CNRM, CNRS UMR 3589, 42 avenue Gaspard Coriolis,
31057 Toulouse, France
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Cited
15 citations as recorded by crossref.
- Control of the temperature signal in Antarctic proxies by snowfall dynamics A. Servettaz et al. 10.5194/tc-17-5373-2023
- Antarctic Ice Cloud Identification and Properties Using Downwelling Spectral Radiance From 100 to 1,400 cm−1 T. Maestri et al. 10.1029/2018JD029205
- In Situ VTOL Drone-Borne Observations of Temperature and Relative Humidity over Dome C, Antarctica P. Ricaud et al. 10.3390/drones7080532
- Ice fog observed at cirrus temperatures at Dome C, Antarctic Plateau É. Vignon et al. 10.5194/acp-22-12857-2022
- Modeling the Dynamics of the Atmospheric Boundary Layer Over the Antarctic Plateau With a General Circulation Model E. Vignon et al. 10.1002/2017MS001184
- Supercooled liquid water cloud observed, analysed, and modelled at the top of the planetary boundary layer above Dome C, Antarctica P. Ricaud et al. 10.5194/acp-20-4167-2020
- Transitions in the wintertime near‐surface temperature inversion at Dome C, Antarctica P. Baas et al. 10.1002/qj.3450
- MODIS-Derived Arctic Melt Season Fog and Low Stratus over East Greenland Glaciers and the Ice Sheet H. Jiskoot et al. 10.1080/07038992.2019.1635878
- 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
- Future Antarctic snow accumulation trend is dominated by atmospheric synoptic-scale events Q. Dalaiden et al. 10.1038/s43247-020-00062-x
- Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses P. Ricaud et al. 10.3390/atmos11080836
- Dependence of the isotopic composition of different precipitation types on air temperature in Central Antarctica N. Tebenkova et al. 10.30758/0555-2648-2021-67-4-368-381
- 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
- Radiatively Induced Precipitation Formation in Diamond Dust X. Zeng 10.1029/2018MS001382
- Antarctic Cloud Macrophysical, Thermodynamic Phase, and Atmospheric Inversion Coupling Properties at McMurdo Station: I. Principal Data Processing and Climatology I. Silber et al. 10.1029/2018JD028279
15 citations as recorded by crossref.
- Control of the temperature signal in Antarctic proxies by snowfall dynamics A. Servettaz et al. 10.5194/tc-17-5373-2023
- Antarctic Ice Cloud Identification and Properties Using Downwelling Spectral Radiance From 100 to 1,400 cm−1 T. Maestri et al. 10.1029/2018JD029205
- In Situ VTOL Drone-Borne Observations of Temperature and Relative Humidity over Dome C, Antarctica P. Ricaud et al. 10.3390/drones7080532
- Ice fog observed at cirrus temperatures at Dome C, Antarctic Plateau É. Vignon et al. 10.5194/acp-22-12857-2022
- Modeling the Dynamics of the Atmospheric Boundary Layer Over the Antarctic Plateau With a General Circulation Model E. Vignon et al. 10.1002/2017MS001184
- Supercooled liquid water cloud observed, analysed, and modelled at the top of the planetary boundary layer above Dome C, Antarctica P. Ricaud et al. 10.5194/acp-20-4167-2020
- Transitions in the wintertime near‐surface temperature inversion at Dome C, Antarctica P. Baas et al. 10.1002/qj.3450
- MODIS-Derived Arctic Melt Season Fog and Low Stratus over East Greenland Glaciers and the Ice Sheet H. Jiskoot et al. 10.1080/07038992.2019.1635878
- 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
- Future Antarctic snow accumulation trend is dominated by atmospheric synoptic-scale events Q. Dalaiden et al. 10.1038/s43247-020-00062-x
- Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses P. Ricaud et al. 10.3390/atmos11080836
- Dependence of the isotopic composition of different precipitation types on air temperature in Central Antarctica N. Tebenkova et al. 10.30758/0555-2648-2021-67-4-368-381
- 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
- Radiatively Induced Precipitation Formation in Diamond Dust X. Zeng 10.1029/2018MS001382
- Antarctic Cloud Macrophysical, Thermodynamic Phase, and Atmospheric Inversion Coupling Properties at McMurdo Station: I. Principal Data Processing and Climatology I. Silber et al. 10.1029/2018JD028279
Latest update: 18 Apr 2024
Short summary
The novelty of the paper is to combine a large set of measurements and meteorological models to study the genesis of thick cloud and diamond dust/ice fog (ice crystals) episodes above Dome C, Antarctica. The originality of the work is to attribute the presence of thick cloud and diamond dust/ice fog to advection and microphysical processes with oceanic and continental origin of air masses, respectively. Thick cloud episodes are reproduced by the models but not diamond dust/ice fog episode.
The novelty of the paper is to combine a large set of measurements and meteorological models to...
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