Observational Analysis of a Southwest Vortex-Induced Severe Rainfall Event Triggering Fatal Landslides over Southwest China in 2024
Open Access
- 5 March 2026
- journal article
- research article
- Published by MDPI AG in Atmosphere
- Vol. 17 (3) , 273
Abstract
In July 2024, a severe rainfall event struck Sichuan Province, Southwest China, triggering deadly landslides and causing significant societal impacts. This study investigates the spatiotemporal characteristics and underlying mechanisms of the event using high-resolution surface observations, radar reflectivity, and ERA5 reanalysis data. The rainfall exhibited distinct mesoscale organization, with two primary precipitation centers identified: subregion A located within the plateau-lain transitional zone of the western Sichuan Basin, and subregion B situated over the Chengdu Plain. Synoptic-scale analysis indicated that the rainfall developed under favorable large-scale atmospheric conditions, including a mid-tropospheric trough, a pronounced low-level jet, and a well-defined Southwest Vortex (SWV), which is a dominant lower-tropospheric circulation system in this region. The evolution of rainfall was closely tied to the initiation and subsequent eastward progression of the SWV. The rainfall-producing mesoscale convective system (MCS) first formed over subregion A at approximately 2300 BST (UTC + 8) on 19 July. Vorticity budget diagnostics revealed that vertical advection and low-level convergence significantly contributed to vortex intensification during this initial phase, closely associated with the orographic lifting of low-level airflow. Convective activity in subregion B commenced roughly four hours later, coinciding with the eastward propagation of the SWV, during which horizontal vorticity advection became the primary mechanism sustaining the vortex. After 1400 BST on 20 July, the SWV weakened significantly, leading to the dissipation of the MCS and the cessation of rainfall.Keywords
Funding Information
- Natural Science Foundation of Sichuan Province (2024NSFSC0776)
- Yunnan Fundamental Research Projects (202501AT070383)
- the Open Fund Project of Key Laboratory of Intelligent Meteorological Observation Technology, China Meteorological Administration (ZNGC2024ZD12)
- the Open Project Fund of the China Meteorological Administration Basin Heavy Rainfall Key Laboratory (2023BHR-Y08)
- the Clinical Science Research Fund of Chengdu Medical College and Ya’an People’s Hospital (24LHXX1-09)
This publication has 26 references indexed in Scilit:
- Dynamic and thermodynamic characteristics of warm-sector rainstorms caused by the southwest china vortex in sichuan basinTheoretical and Applied Climatology, 2024
- Case study on the formation of a torrential‐rainfall‐producing southwest vortex: Backward trajectory analyses and sensitivity simulationsAtmospheric Science Letters, 2024
- General features and synoptic-scale environments of mesoscale convective systems over South China during the 2013–2017 pre-summer rainy seasonsAtmospheric Research, 2022
- The ERA5 global reanalysisQuarterly Journal of the Royal Meteorological Society, 2020
- Comparison of the movement and vertical structures of two types of the southwest vortexMeteorology and Atmospheric Physics, 2019
- Causes of extreme rainfall in May 2013 over Henan Province: the role of the southwest vortex and low-level jetTheoretical and Applied Climatology, 2017
- Mesoscale observational analysis of lifting mechanism of a warm-sector convective system producing the maximal daily precipitation in China mainland during pre-summer rainy season of 2015Journal of Meteorological Research, 2016
- Observational facts regarding the joint activities of the southwest vortex and plateau vortex after its departure from the Tibetan PlateauAdvances in Atmospheric Sciences, 2015
- Investigation of the predictability and physical mechanisms of an extreme-rainfall-producing mesoscale convective system along the Meiyu front in East China: An ensemble approachJournal of Geophysical Research: Atmospheres, 2015
- Vorticity budget investigation of a simulated long-lived mesoscale vortex in South ChinaAdvances in Atmospheric Sciences, 2004