July 14, 2025Open Access

Distinct Microphysical Characteristics of Ice Particles in Convective versus Stratiform Regions of Stratocumulus Clouds: A Case Study

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Authors

ZSZ-X ShenTongji University XLXiaoli LiuChina Meteorological Administration YLYan LiChinese Academy of Sciences

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Implication

Case study analyzes microphysical differences between ice particles in convective and stratiform zones of stratocumulus clouds, indicating varied precipitation mechanisms.

Key Points

MAIN FINDING: Ice particles in convective regions have larger and denser characteristics compared to those in stratiform regions.
KEY EVIDENCE: Maximum rime density in convective areas reaches 0.55 g cm-3, while stratiform regions show weaker riming effects.
APPROACH: The research uses airborne data, mesoscale simulations, and particle-based modeling to examine cloud events in northern China.
SIGNIFICANCE: Understanding these microphysical differences enhances knowledge of precipitation processes in stratocumulus clouds.

Cite This Study

Shen et al. (2025) studied this question.

synapsesocial.com/papers/689a02b6e6551bb0af8cc3d1 https://doi.org/10.5194/egusphere-2025-3034

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Implication

Case study analyzes microphysical differences between ice particles in convective and stratiform zones of stratocumulus clouds, indicating varied precipitation mechanisms.

Distinct Microphysical Characteristics of Ice Particles in Convective versus Stratiform Regions of Stratocumulus Clouds: A Case Study

Discussion

Member takes

Implication

Key Points

Cite This Study

Distinct Microphysical Characteristics of Ice Particles in Convective versus Stratiform Regions of Stratocumulus Clouds: A Case Study

Discussion

Member takes

Implication

Key Points

Cite This Study

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