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Meso-γ-scale dynamic and thermodynamic mechanisms in an extreme rainfall event in Zhengzhou, China

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The study showed that dynamic acceleration was crucial for convection below 4 km, sustaining heavy rainfall.
Unique mechanisms for maintaining quasi-stationary convection under weak cold-pool conditions were identified.
Findings indicated that low-level vertical wind shear significantly influenced the meso-γ-scale vortex and updraft behavior.
This research enhances our understanding of storm-scale processes and their role in extreme rainfall events.

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Weather Research and Forecasting simulation reveals key dynamic acceleration and thermodynamic mechanisms in extreme rainfall events.

Li et al. (2025) studied this question.

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