Hu et al. (2025) Long-term changes in the drought propagation characteristics in the Yangtze River Basin
Identification
- Journal: Journal of Hydrology Regional Studies
- Year: 2025
- Date: 2025-12-11
- Authors: R. Hu, Shanshui Yuan, Junliang Jin, Liujun Zhu, Yi Liu
- DOI: 10.1016/j.ejrh.2025.103014
Research Groups
- State Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing, China
- Yangtze Institute for Conservation and Development, Hohai University, Nanjing, China
- College of Hydrology and Water Resources, Hohai University, Nanjing, China
Short Summary
This study systematically assesses the long-term evolution of drought propagation characteristics in the Yangtze River Basin (1950–2022) using a dynamic sliding-window framework and copula-based joint probability analysis. It reveals significant spatiotemporal changes in drought propagation time and risk, highlighting the influence of vegetation type and hydrological interventions.
Objective
- To systematically quantify the long-term evolutionary trends of drought propagation time and risk from meteorological to agricultural and hydrological droughts in the Yangtze River Basin over the past decades.
- To identify the spatial patterns of these trends and explore potential climatic or anthropogenic factors associated with these changes.
Study Configuration
- Spatial Scale: Yangtze River Basin, covering approximately 1.8 million square kilometers (24°27’ - 35°54’ N, 90°33’ - 122°19’ E).
- Temporal Scale: 1950–2022 (73 years), analyzed using a 30-year sliding-window framework.
Methodology and Data
- Models used:
- Standardized Precipitation Index (SPI)
- Standardized Soil Moisture Index (SSI)
- Standardized Runoff Index (SRI)
- Pearson Correlation Coefficient (PCC) for Drought Propagation Time (DPT)
- Copula functions (Gaussian, Gumbel, Frank) for joint probability analysis of drought duration and severity
- Drought Hazard Propagation Ratio (DHPR)
- Mann-Kendall trend test for temporal trends
- Data sources: ERA5-Land dataset (precipitation, soil moisture, runoff) with a spatial resolution of 0.1° from 1950 to 2022.
Main Results
- Drought propagation from meteorological drought (MD) to agricultural drought (AD) is predominantly characterized by a 2-month lag across 64.5 % of the basin.
- MD to hydrological drought (HD) propagation typically exhibits a 4-month lag, with approximately 25 % of the basin experiencing lags exceeding 6 months.
- Sliding-window analysis reveals significant decreases in DPT in parts of the upper basin, but widespread increases in drought propagation risk, particularly in the Sichuan Basin.
- Areas dominated by cultivated vegetation show longer propagation times and higher risks, with more pronounced upward trends compared to natural vegetation regions.
- For MD-AD propagation, the DHPR for severity tends to decrease with increasing return periods (e.g., 61.5 % of the basin has DHPR < 1.0 at a 100-year return period), while the DHPR for duration increases.
- For MD-HD propagation, both severity and duration DHPR exhibit a clear increasing trend across nearly the entire basin, with amplification becoming more pronounced at longer return periods (e.g., DHPR (Severity) > 2.0 rises to 14.1 % at a 100-year return period).
- DPT trends for MD-AD are spatially scattered, with significant lengthening in the high-altitude source region (+0.08 month/year) and shortening downstream (-0.10 month/year).
- DPT trends for MD-HD are more spatially coherent, showing widespread significant shortening in the upper reaches (-0.04 to -0.10 month/year) and lengthening in the source region and parts of the middle reaches (+0.04 to +0.08 month/year).
Contributions
- Provides a novel dynamic assessment of long-term evolutionary trends in drought propagation characteristics (time and risk) in a large river basin, moving beyond static analyses.
- Systematically quantifies these trends using a 30-year sliding-window framework combined with copula-based joint probability analysis.
- Clarifies the spatiotemporal patterns and the role of vegetation types in controlling drought propagation dynamics.
- Offers critical regional knowledge for developing proactive and adaptive drought early warning systems and water resource management strategies.
- Highlights the non-linear response of drought propagation to extreme events and the distinct propagation mechanisms between agricultural and hydrological pathways.
Funding
- National Key Research and Development Program of China (2023YFC3209800)
- Basic Research Project of Jiangsu Province (BK20250090)
- National Natural Science Foundation of China (52279011)
Citation
@article{Hu2025Longterm,
author = {Hu, R. and Yuan, Shanshui and Jin, Junliang and Zhu, Liujun and Liu, Yi},
title = {Long-term changes in the drought propagation characteristics in the Yangtze River Basin},
journal = {Journal of Hydrology Regional Studies},
year = {2025},
doi = {10.1016/j.ejrh.2025.103014},
url = {https://doi.org/10.1016/j.ejrh.2025.103014}
}
Original Source: https://doi.org/10.1016/j.ejrh.2025.103014