Remote sensing-based monitoring of compound drought-waterlogging stress in groundwater-sensitive agroecosystems in arid regions

Groundwater-Sensitive Agroecosystem (GWSA) in arid regions are increasingly vulnerable to compound drought-waterlogging disasters driven by groundwater fluctuations under climate change. This study proposes a remote sensing-based framework to monitor such compound stress in the Gahai Irrigation District, Northwest China. By integrating a 1 km-resolution root-zone soil moisture (RZSM) dataset with 33 downscaling factors (e.g., vegetation indices, topography, and hydrological variables), we generated a 30 m-resolution daily RZSM product (2018–2022) using a Random Forest algorithm. The Soil Moisture Condition Index (SMCI-index) and Double Stress Index (DSI) were developed to identify drought (SMCI-index < 0.4 for ≥10 days) and waterlogging (SMCI-index > 0.6 for ≥3 days) events and their synergistic impacts. Results revealed significant spatial heterogeneity in Compound Drought-Waterlogging Stress: moderate stress dominated central GWSA (13.82 km²), driven by waterlogging-induced soil degradation, while severe stress (6.04 km²) occurred along boundaries with alternating drought-waterlogging dominance. Groundwater level, precipitation, and temperature were key drivers, with temperature paradoxically reducing drought areas via snowmelt-enhanced recharge. Validation of the SMCI-index derived from RZSM data showed strong consistency with vegetation indices (POD > 80 %, r = 0.98) and a 69.27 % spatial overlap with modeled waterlogging zones. This study demonstrates that the use of downscaled RZSM data can effectively mitigate precipitation interference and enable fine-scale monitoring of groundwater-driven compound drought-waterlogging stress. The findings offer critical insights for enhancing agricultural resilience and thus maintaining ecosystem services in GWSA under hydrological extremes. • An RS-based framework was developed to monitor groundwater-driven compound drought-waterlogging stress. • Downscaled RZSM data effectively enabled fine-scale monitoring of groundwater-driven compound drought-waterlogging stress. • Moderate compound stress was found to dominate the central part of the Gahai Irrigation District. • Groundwater level and temperature were key drivers of compound drought-waterlogging stress.

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Publication Details

Journal
Agricultural Water Management
Published
2025-09-22
DOI
https://doi.org/10.1016/j.agwat.2025.109826
Citations
1
Primary Topic
Hydrology and Drought Analysis
Type
article
Field-Weighted Citation Impact
1.11
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Remote sensing-based monitoring of compound drought-waterlogging stress in groundwater-sensitive agroecosystems in arid regions

Xin Jin, Xufeng Mao, Na Yao, Di Fu et al.
1 citations
Agricultural Water Management
Hydrology and Drought Analysis
1.11
article

Remote sensing-based monitoring of compound drought-waterlogging stress in groundwater-sensitive agroecosystems in arid regions

Xin Jin, Xufeng Mao, Na Yao, Di Fu, Yanxiang Jin
article en
1 citations

Abstract

Groundwater-Sensitive Agroecosystem (GWSA) in arid regions are increasingly vulnerable to compound drought-waterlogging disasters driven by groundwater fluctuations under climate change. This study proposes a remote sensing-based framework to monitor such compound stress in the Gahai Irrigation District, Northwest China. By integrating a 1 km-resolution root-zone soil moisture (RZSM) dataset with 33 downscaling factors (e.g., vegetation indices, topography, and hydrological variables), we generated a 30 m-resolution daily RZSM product (2018–2022) using a Random Forest algorithm. The Soil Moisture Condition Index (SMCI-index) and Double Stress Index (DSI) were developed to identify drought (SMCI-index < 0.4 for ≥10 days) and waterlogging (SMCI-index > 0.6 for ≥3 days) events and their synergistic impacts. Results revealed significant spatial heterogeneity in Compound Drought-Waterlogging Stress: moderate stress dominated central GWSA (13.82 km²), driven by waterlogging-induced soil degradation, while severe stress (6.04 km²) occurred along boundaries with alternating drought-waterlogging dominance. Groundwater level, precipitation, and temperature were key drivers, with temperature paradoxically reducing drought areas via snowmelt-enhanced recharge. Validation of the SMCI-index derived from RZSM data showed strong consistency with vegetation indices (POD > 80 %, r = 0.98) and a 69.27 % spatial overlap with modeled waterlogging zones. This study demonstrates that the use of downscaled RZSM data can effectively mitigate precipitation interference and enable fine-scale monitoring of groundwater-driven compound drought-waterlogging stress. The findings offer critical insights for enhancing agricultural resilience and thus maintaining ecosystem services in GWSA under hydrological extremes. • An RS-based framework was developed to monitor groundwater-driven compound drought-waterlogging stress. • Downscaled RZSM data effectively enabled fine-scale monitoring of groundwater-driven compound drought-waterlogging stress. • Moderate compound stress was found to dominate the central part of the Gahai Irrigation District. • Groundwater level and temperature were key drivers of compound drought-waterlogging stress.

Agricultural Water ManagementVol. 319
Openalex Percentile: Top 19%
Hydrology and Drought Analysis
1.11
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