Zou et al. (2026) Linking agricultural drought to compound hot–dry risk: A process-based compound index for crop and water management in the North China Plain
Identification
- Journal: Agricultural Water Management
- Year: 2026
- Date: 2026-09-22
- Authors: Yi Zou, Ruiyuan Pan, Shaowei Ning, Xiangyu Li, Yuliang Zhou, Xiaoyan Xu, Zihao Zheng, Le Chen, Kaixuan Zhang, Lichang Xu
- DOI: 10.1016/j.agwat.2026.110796
Research Groups
- College of Civil Engineering, Hefei University of Technology
- Joint Laboratory of Artificial Intelligence for Water Security, Hefei University of Technology
- Aerospace Information Research Institute, Chinese Academy of Sciences
- School of Geography and Planning, Sun Yat-sen University
Short Summary
This study develops a Copula-based Compound Hot-Dry Index (CHDI) to characterize compound hot-dry events in the North China Plain. The CHDI integrates meteorological drought, agricultural drought, and high-temperature anomalies into a unified probabilistic framework.
Objective
- Investigate the spatiotemporal evolution and phase-dependent driving mechanisms of compound hot-dry events during 1980–2022.
- Characterize the dependence structure among meteorological drought, agricultural drought, and high-temperature anomalies using Copula-based joint modeling.
Study Configuration
- Spatial Scale: The study area is located in the North China Plain, covering an area of approximately 300,000 km².
- Temporal Scale: The temporal scale ranges from 1980 to 2022, with a focus on the period 2000–2022 for detailed analysis.
Methodology and Data
- Models used: Copula-based joint modeling (Gaussian Copula, t Copula, Frank Copula, Clayton Copula, Gumbel Copula) was used to model the multivariate dependence structure among SPEI, SSI, and STI.
- Data sources:
- Meteorological variables (temperature, precipitation, surface pressure, relative humidity, wind speed, potential evapotranspiration) from the National Cryosphere Desert Data Center.
- Hydrothermal indicators (SPEI, SSI, STI) derived from Zhang et al. (2025a).
- NDVI data obtained from the GIMMS NDVI global long-term vegetation dataset archived by the ORNL DAAC.
- Root-zone soil moisture data obtained from the GLEAM4 dataset.
- Runoff data derived from the ERA5-Land dataset acquired through the Google Earth Engine platform.
- Solar radiation data obtained from the National Tibetan Plateau Data Center.
Main Results
- The CHDI was found to accurately identify the occurrence timing, spatial extent, and month-to-month evolution of typical events.
- The results show that CHDI exhibits stronger consistency with anomalies in agricultural vegetation productivity compared to existing indices.
- Over the past four decades, compound hot-dry conditions in the North China Plain have intensified overall, with CHDI decreasing at a rate of approximately −0.111 per decade.
Contributions
- This study extends the characterization framework of compound events by integrating meteorological drought, agricultural drought, and high-temperature anomalies into a unified probabilistic framework.
- The CHDI provides a more comprehensive representation of the integrity and continuity of compound hot-dry processes.
Funding
- National Natural Science Foundation of China (Grant No. 51979017)
- National Key Research and Development Program of China (Grant No. 2018YFC1504204)
Citation
@article{Zou2026Linking,
author = {Zou, Yi and Pan, Ruiyuan and Ning, Shaowei and Li, Xiangyu and Zhou, Yuliang and Xu, Xiaoyan and Zheng, Zihao and Chen, Le and Zhang, Kaixuan and Xu, Lichang},
title = {Linking agricultural drought to compound hot–dry risk: A process-based compound index for crop and water management in the North China Plain},
journal = {Agricultural Water Management},
year = {2026},
doi = {10.1016/j.agwat.2026.110796},
url = {https://doi.org/10.1016/j.agwat.2026.110796}
}
Original Source: https://doi.org/10.1016/j.agwat.2026.110796