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.
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
16 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
- 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
- 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
16 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
- 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
- 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: 20 Nov 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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