Articles | Volume 24, issue 23
https://doi.org/10.5194/acp-24-13429-2024
© Author(s) 2024. 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-24-13429-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Microphysical view of the development and ice production of mid-latitude stratiform clouds with embedded convection during an extratropical cyclone
Yuanmou Du
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang, 310027, China
Delong Zhao
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Mengyu Huang
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Ping Tian
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Dian Wen
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Wei Xiao
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Wei Zhou
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Hui He
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Baiwan Pan
Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang, 310027, China
Dongfei Zuo
CMA Weather Modification Center, Beijing, 100081, China
Xiange Liu
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Yingying Jing
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Rong Zhang
CMA Weather Modification Center, Beijing, 100081, China
Jiujiang Sheng
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Fei Wang
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Yu Huang
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Yunbo Chen
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
Deping Ding
Beijing Weather Modification Center, Beijing, 100089, China
Beijing Key Laboratory of Cloud, Precipitation and Atmospheric Water Resources, Beijing, 100089, China
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Short summary
By conducting in situ measurements, we investigated ice production processes in stratiform clouds with embedded convection over the North China Plain. The results show that the ice number concentration is strongly related to the distance to the cloud top, and the level with a larger distance to the cloud top has more graupel falling from upper levels, which promotes collision and coalescence between graupel and droplets and enhances secondary ice production.
By conducting in situ measurements, we investigated ice production processes in stratiform...
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