Analyzes the effects of vapor pressure deficit on maize water productivity across various climate scenarios, indicating potential risks for crop yield management.
Maize production is highly vulnerable to rising vapor pressure deficit (VPD), yet its agricultural-scale impacts remain insufficiently characterized due to the lack of integrated assessments linking spatiotemporal VPD dynamics with crop-level water productivity (WP), particularly the relative contributions of yield and evapotranspiration (ET) under varying atmospheric drought conditions. Using the Coupled Model Intercomparison Project Phase 6 (CMIP6) data, we analyzed the spatiotemporal evolution of VPD across five maize ecoregions in the Yellow River Basin (YRB) under three Shared Socioeconomic Pathway (SSP) scenarios (baseline: 1985–2014; future: 2021–2100) and quantified its effects on maize WP. Mean VPD across the YRB maize ecoregions is projected to increase by 21% from 2021 to 2100 (vs. 1985–2014), peaking in the 2080 s under SSP585. Eastern ecoregions (II > I) experience greater VPD escalation than western counterparts (V > III > IV), with post-2030s VPD growth accelerating to 0.036 kPa/yr under SSP585, while SSP126 stabilizes. Projected VPD increases may hinder WP sustainability in regions II-V across all climate scenarios. ET primarily governs WP under mild atmospheric drought (VPD ≤ 4 kPa), whereas yield constraints dominate under severe drought. Thus, a VPD-dependent shift in the WP demands a process-based optimization of irrigation and yield management under varying atmospheric drought conditions and offers actionable insights for climate-resilient agricultural strategies in (semi-)arid maize-growing regions. • Vapor pressure deficit is projected to increase by 21% across maize regions in the Yellow River Basin. • Eastern regions show faster increases in atmospheric dryness than western regions under future scenarios. • High vapor pressure deficit increases the frequency of low water productivity years. • Water productivity shifts from evapotranspiration control to yield limitation beyond 4 kPa. • Yield-limited water productivity shows higher sensitivity to vapor pressure deficit.
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Chen et al. (2026) studied this question.
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