Articles | Volume 19, issue 2
Atmos. Chem. Phys., 19, 877–886, 2019
https://doi.org/10.5194/acp-19-877-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 877–886, 2019
https://doi.org/10.5194/acp-19-877-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article 23 Jan 2019
Research article | 23 Jan 2019
New type of evidence for secondary ice formation at around −15 °C in mixed-phase clouds
Claudia Mignani et al.
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Cited
10 citations as recorded by crossref.
- Biological Ice-Nucleating Particles Deposited Year-Round in Subtropical Precipitation R. Joyce et al. 10.1128/AEM.01567-19
- Spatial and temporal variability in the ice-nucleating ability of alpine snowmelt and extension to frozen cloud fraction K. Brennan et al. 10.5194/acp-20-163-2020
- Using freezing spectra characteristics to identify ice-nucleating particle populations during the winter in the Alps J. Creamean et al. 10.5194/acp-19-8123-2019
- The impact of secondary ice production on Arctic stratocumulus G. Sotiropoulou et al. 10.5194/acp-20-1301-2020
- Towards parameterising atmospheric concentrations of ice-nucleating particles active at moderate supercooling C. Mignani et al. 10.5194/acp-21-657-2021
- Secondary Ice Formation in Idealised Deep Convection—Source of Primary Ice and Impact on Glaciation A. Miltenberger et al. 10.3390/atmos11050542
- Microphysical investigation of the seeder and feeder region of an Alpine mixed-phase cloud F. Ramelli et al. 10.5194/acp-21-6681-2021
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Development of the drop Freezing Ice Nuclei Counter (FINC), intercomparison of droplet freezing techniques, and use of soluble lignin as an atmospheric ice nucleation standard A. Miller et al. 10.5194/amt-14-3131-2021
- Continuous online monitoring of ice-nucleating particles: development of the automated Horizontal Ice Nucleation Chamber (HINC-Auto) C. Brunner & Z. Kanji 10.5194/amt-14-269-2021
10 citations as recorded by crossref.
- Biological Ice-Nucleating Particles Deposited Year-Round in Subtropical Precipitation R. Joyce et al. 10.1128/AEM.01567-19
- Spatial and temporal variability in the ice-nucleating ability of alpine snowmelt and extension to frozen cloud fraction K. Brennan et al. 10.5194/acp-20-163-2020
- Using freezing spectra characteristics to identify ice-nucleating particle populations during the winter in the Alps J. Creamean et al. 10.5194/acp-19-8123-2019
- The impact of secondary ice production on Arctic stratocumulus G. Sotiropoulou et al. 10.5194/acp-20-1301-2020
- Towards parameterising atmospheric concentrations of ice-nucleating particles active at moderate supercooling C. Mignani et al. 10.5194/acp-21-657-2021
- Secondary Ice Formation in Idealised Deep Convection—Source of Primary Ice and Impact on Glaciation A. Miltenberger et al. 10.3390/atmos11050542
- Microphysical investigation of the seeder and feeder region of an Alpine mixed-phase cloud F. Ramelli et al. 10.5194/acp-21-6681-2021
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Development of the drop Freezing Ice Nuclei Counter (FINC), intercomparison of droplet freezing techniques, and use of soluble lignin as an atmospheric ice nucleation standard A. Miller et al. 10.5194/amt-14-3131-2021
- Continuous online monitoring of ice-nucleating particles: development of the automated Horizontal Ice Nucleation Chamber (HINC-Auto) C. Brunner & Z. Kanji 10.5194/amt-14-269-2021
Latest update: 30 Jul 2021
Short summary
A snow crystal can be generated from an ice nucleating particle or from an ice splinter. In this study we made use of the fact that snow crystals with a particular shape (dendrites) grow within a narrow temperature range (−12 to −17 °C) and can be analysed individually for the presence of an ice nucleating particle. Our direct approach revealed that only one in eight crystals contained such a particle and was of primary origin. The other crystals must have grown from ice splinters.
A snow crystal can be generated from an ice nucleating particle or from an ice splinter. In this...
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