Articles | Volume 17, issue 8
Atmos. Chem. Phys., 17, 5221–5237, 2017
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.
Atmos. Chem. Phys., 17, 5221–5237, 2017
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
Philippe Ricaud et al.
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Cited
11 citations as recorded by crossref.
- Transitions in the wintertime near‐surface temperature inversion at Dome C, Antarctica P. Baas et al. 10.1002/qj.3450
- Antarctic Ice Cloud Identification and Properties Using Downwelling Spectral Radiance From 100 to 1,400 cm −1 T. Maestri et al. 10.1029/2018JD029205
- 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
- Modeling the Dynamics of the Atmospheric Boundary Layer Over the Antarctic Plateau With a General Circulation Model E. Vignon et al. 10.1002/2017MS001184
- 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
- Radiatively Induced Precipitation Formation in Diamond Dust X. Zeng 10.1029/2018MS001382
- Observing and Modeling Ice Sheet Surface Mass Balance J. Lenaerts et al. 10.1029/2018RG000622
- AWARE: The Atmospheric Radiation Measurement (ARM) West Antarctic Radiation Experiment D. Lubin et al. 10.1175/BAMS-D-18-0278.1
- 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
- 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
11 citations as recorded by crossref.
- Transitions in the wintertime near‐surface temperature inversion at Dome C, Antarctica P. Baas et al. 10.1002/qj.3450
- Antarctic Ice Cloud Identification and Properties Using Downwelling Spectral Radiance From 100 to 1,400 cm −1 T. Maestri et al. 10.1029/2018JD029205
- 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
- Modeling the Dynamics of the Atmospheric Boundary Layer Over the Antarctic Plateau With a General Circulation Model E. Vignon et al. 10.1002/2017MS001184
- 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
- Radiatively Induced Precipitation Formation in Diamond Dust X. Zeng 10.1029/2018MS001382
- Observing and Modeling Ice Sheet Surface Mass Balance J. Lenaerts et al. 10.1029/2018RG000622
- AWARE: The Atmospheric Radiation Measurement (ARM) West Antarctic Radiation Experiment D. Lubin et al. 10.1175/BAMS-D-18-0278.1
- 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
- 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
Latest update: 04 Mar 2021
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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