Two types of heavy rainfall, namely warm-sector and frontal heavy rainfall, coexist in South
China during the presummer rainy season and manifest as varying mechanisms and …

Inland frontal heavy rainfall (FR) and coastal warm‐sector heavy rainfall (WR) are two typical
types of precipitation in South China during the pre‐summer rainy season. FR and WR are …

The northern mountainous area of the Pearl River Delta (PRD) is a center of convection and
heavy rainfall of coastal southern China during the summer monsoon season. Although …

Abstract Coastal South China is frequently exposed to substantial rainfall within fronts-free
environments during the presummer rainy season, which recurrently leads to severe …

A local long-lived convective system developed at midnight over inland South China,
producing record-breaking rainfall in Guangzhou on 7 May 2017. This study examines the …

Extreme precipitation events have been occurring frequently worldwide, and their causative
factors and convection initiation (CI) mechanisms have been attracting more and more …

This study analyzes general features and circulation patterns of 98 quasi-linear meso-scale
convective systems (MCSs) over South China (SC) during May 1 to June 15, 2013–2017 …

Convectively generated cold pools play a crucial role in the convection initiation and
development, but observations of their vertical structure are insufficient. In this study …

A series of convection‐permitting numerical experiments using the Weather Research and
Forecasting Model with different model configurations are performed to investigate physical …

Warm-sector heavy rainfall in southern China refers to the heavy rainfall that occurs within a
weakly forced synoptic environment under the influence of monsoonal airflows. It is usually …