Deng et al. (2026) Assessing the climatic effects and feedback mechanisms of large-scale crop irrigation using the improved WRF model
Identification
- Journal: Agricultural Water Management
- Year: 2026
- Date: 2026-07-29
- Authors: Haodong Deng, Yu Wang, Chaoqun Li, Qingming Wang, Fusheng Li, Dengming Yan, Xiaoxue Chen, Kai HOU, Mingkun Sun, Xie Lian
- DOI: 10.1016/j.agwat.2026.110670
Research Groups
- Yellow River Engineering Consulting Co., Ltd.
- Key Laboratory of Water Management and Water Security for Yellow River Basin, Ministry of Water Resources
- State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research
- Henan Water & Power Engineering Consulting CO., Ltd, Henan Water Conservancy Investment Group CO., Ltd
Short Summary
This study investigates the climatic effects and underlying mechanisms of large-scale crop irrigation (LSCI) in the Huanghe-Huaihe-Haihe River (HHH) basin using the Weather Research and Forecasting (WRF) model. The results show that LSCI significantly modifies surface water and energy balances, leading to a 2.85% increase in evapotranspiration, a 0.19°C reduction in near-surface temperature, and a 5.29 mm increase in precipitation.
Objective
- Investigate the climatic effects of large-scale crop irrigation (LSCI) on regional climate elements in the Huanghe-Huaihe-Haihe River (HHH) basin.
- Quantify the underlying mechanisms driving these climate effects from perspectives such as water vapor transport against the monsoon background.
Study Configuration
- Spatial Scale: The study focuses on the HHH basin, which spans from 95°E to 124°E and from 30°N to 43°N, covering a total land area of 1.385 million km².
- Temporal Scale: The simulation period spans from 2001 to 2022.
Methodology and Data
- Models used: Weather Research and Forecasting (WRF) model coupled with an improved Noah-MP land surface scheme.
- Data sources: ERA5 reanalysis data, municipal-level statistical irrigation water volumes, and land use datasets.
Main Results
- LSCI leads to a 2.85% increase in evapotranspiration, a 0.19°C reduction in near-surface temperature, and a 5.29 mm increase in precipitation.
- The horizontal water vapor flux increases by 0.15 kg⋅m−1⋅s−1 annually, with the most significant enhancements observed in spring and summer.
- The vertical water vapor flux increases by 0.05 kg⋅m−1⋅s−1 annually, with the most significant enhancements observed in spring and summer.
Contributions
- This study provides new insights into irrigation climate interactions and offers a scientific basis for understanding land-atmosphere feedback mechanisms.
- The refined irrigation scheme used in this study improves the representation of irrigation water volumes, spatial allocation, and physical infiltration processes.
Funding
- This research was funded by [project 1], [project 2], and [project 3].
Citation
@article{Deng2026Assessing,
author = {Deng, Haodong and Wang, Yu and Li, Chaoqun and Wang, Qingming and Li, Fusheng and Yan, Dengming and Chen, Xiaoxue and HOU, Kai and Sun, Mingkun and Lian, Xie},
title = {Assessing the climatic effects and feedback mechanisms of large-scale crop irrigation using the improved WRF model},
journal = {Agricultural Water Management},
year = {2026},
doi = {10.1016/j.agwat.2026.110670},
url = {https://doi.org/10.1016/j.agwat.2026.110670}
}
Original Source: https://doi.org/10.1016/j.agwat.2026.110670