Wang et al. (2025) Polarised Changes in Sub‐Daily Precipitation Extremes and Underlying Mechanisms Over Southwest China in a Warmer Climate
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: International Journal of Climatology
- Year: 2025
- Date: 2025-10-05
- Authors: Yujie Wang, Lianchun Song, Pengke Shen
- DOI: 10.1002/joc.70140
Research Groups
Not specified in the abstract.
Short Summary
This study statistically analyzed sub-daily precipitation extremes (SPEs) over Southwest China from 1971–2024, revealing simultaneous increases in both wet and dry SPEs driven by atmospheric circulation changes and thermodynamic factors in a warming climate.
Objective
- To statistically analyze spatiotemporal variations of sub-daily precipitation extremes (SPEs) over Southwest China and identify the underlying mechanisms driving their polarized changes (simultaneous increases in both wet and dry extremes).
Study Configuration
- Spatial Scale: Southwest China (SWC)
- Temporal Scale: Summers of 1971–2024
Methodology and Data
- Models used: Statistical analysis methods.
- Data sources: Observation data from 338 meteorological stations.
Main Results
- Sub-daily precipitation extremes (SPEs) exhibit simultaneous increases in both wet and dry extremes across Southwest China.
- The SPE risks for 20-year and 50-year return periods increased by 2–8 times and 4–17 times, respectively, in 2001–2024 compared to 1971–2000.
- Precipitation intensity at 1–3 hour intervals shows a more pronounced upward trend (3.4% per decade) than at 6–12 hour intervals (2.7% per decade).
- Wet SPEs show a nearly consistent upward trend across SWC, with larger magnitudes in Chongqing, southern Sichuan, and southern Yunnan.
- Remarkable increases in dry SPEs occur in Yunnan and southern Guizhou.
- Enhanced and westward-extended Western Pacific Subtropical High (WPSH), combined with enhanced and eastward-extended South Asian High (SAH), are key factors driving increased wet SPEs.
- Extraordinary westward extension of the WPSH is conducive to forming dry SPEs.
- In a warming climate, increases in saturated vapor pressure, specific humidity, water vapor convergence, and convective available potential energy are associated with substantial increases in wet SPEs.
- Simultaneously, increased saturated vapor pressure makes it more difficult for water vapor to reach saturation, triggering occurrences of dry SPEs.
Contributions
- Provides a scientific basis for decision-makers adapting to sub-daily precipitation extremes.
- Offers valuable insights for further in-depth research on polarized changes in precipitation extremes and their underlying mechanisms.
- Addresses a gap in understanding simultaneous increases in both wet and dry sub-daily precipitation extremes over Southwest China.
Funding
Not specified in the abstract.
Citation
@article{Wang2025Polarised,
author = {Wang, Yujie and Song, Lianchun and Shen, Pengke},
title = {Polarised Changes in Sub‐Daily Precipitation Extremes and Underlying Mechanisms Over Southwest China in a Warmer Climate},
journal = {International Journal of Climatology},
year = {2025},
doi = {10.1002/joc.70140},
url = {https://doi.org/10.1002/joc.70140}
}
Original Source: https://doi.org/10.1002/joc.70140