Articles | Volume 20, issue 3
https://doi.org/10.5194/acp-20-1391-2020
© 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-20-1391-2020
© 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
| 
05 Feb 2020
Research article | Highlight paper |
| 05 Feb 2020
| 05 Feb 2020
A new look at the environmental conditions favorable to secondary ice production
Environment and Climate Change Canada, Toronto, ON, Canada
Ivan Heckman
Environment and Climate Change Canada, Toronto, ON, Canada
Mengistu Wolde
National Research Council, Ottawa, ON, Canada
Andrew S. Ackerman
NASA Goddard Institute for Space Studies, New York, NY, USA
Ann M. Fridlind
NASA Goddard Institute for Space Studies, New York, NY, USA
Luis A. Ladino
Environment and Climate Change Canada, Toronto, ON, Canada
Centro de Ciencias de la Atmósfera, Universidad Nacional Autonoma de Mexico, Mexico City, Mexico
R. Paul Lawson
Stratton Park Engineering Company, Boulder, CO, USA
Jason Milbrandt
Environment and Climate Change Canada, Toronto, ON, Canada
Earle Williams
Massachusetts Institute of Technology, Boston, MA, USA
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Discussed (final revised paper)
Discussed (final revised paper)
Latest update: 22 Apr 2024
Short summary
This study attempts identification of mechanisms of secondary ice production (SIP) based on the observation of small faceted ice crystals. It was found that in both mesoscale convective systems and frontal clouds, SIP was observed right above the melting layer and extended to the higher altitudes with colder temperatures. A principal conclusion of this work is that the freezing drop shattering mechanism is plausibly accounting for the measured ice concentrations in the observed condition.
This study attempts identification of mechanisms of secondary ice production (SIP) based on the...
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