**Background:** Grassland ecosystems cover about one-quarter of Earth's land area and store large quantities of soil organic carbon (SOC). They are critical for fiber, meat, and milk production but also contribute to greenhouse gas emissions. Climate change—through rising CO₂, temperature shifts, altered precipitation, and increased extremes—poses significant uncertainty for grassland productivity and carbon storage. Previous work has shown that SOC stocks are sensitive to land use and management, but long-term projections under integrated climate scenarios remain poorly understood. This study aimed to (1) assess the impacts of changes in key meteorological variables on CO₂ fluxes, grassland and milk productivity, and SOC stocks, and (2) simulate the potential influence of long-term future climate scenarios and extreme events on these variables.
**Methods:** The study used the CenW ecosystem model (version 4.2), a process-based model simulating carbon, water, and nitrogen cycles on a daily time step. The site was located in Lusignan, southwestern France (mean temperature 11.2°C, precipitation 774 mm yr⁻¹). Two management systems were modeled: a mowed paddock (receiving >320 kg N ha⁻¹ yr⁻¹, 3–4 cuts per year) and a rotationally grazed paddock (receiving <50 kg N ha⁻¹ yr⁻¹, grazed 7.4 times per year, stocking rate 17 heads ha⁻¹). The model was previously calibrated and validated using eddy covariance data (2006–2010). Sensitivity analyses tested individual changes: temperature (−4°C to +4°C), precipitation (−25% to +25%), and CO₂ (−15% to +780 ppm). Long-term simulations used three RCP scenarios (RCP 2.6, RCP 4.5, RCP 8.5) from the CNRM2014 experiment, covering 1975–2100 divided into four periods: Historical (H: 1975–2005), Near Future (NF: 2006–2036), Intermediate Future (IF: 2037–2067), and Far Future (FF: 2068–2100). Six ETCCDI extreme climate indices were analyzed: number of hot days (NHD), TX90p, warm spell duration index (WSDI), maximum length of dry spell (MLDS), R95pTOT, and prcpTOT.
**Key Results:** Under factorial changes, increasing temperature slightly increased GPP, NPP, and milk production but strongly reduced SOC (e.g., −16% under +4°C for grazed). Reduced precipitation (−25%) decreased GPP by −14%, milk production by −28%, and NPP by −11%, but SOC increased slightly (+2%). Doubling CO₂ (to 780 ppm) increased GPP by +27%, NPP by +25%, milk production by +91%, and N fertilizer requirements by +65%, while SOC decreased marginally (−1%). Under RCP scenarios with increasing CO₂, GPP in FF increased by 11% (RCP 2.6), 14% (RCP 4.5), and 28% (RCP 8.5) relative to H. Milk production in FF increased by 104% under RCP 8.5. SOC decreased under all scenarios: −2% (RCP 2.6 and RCP 4.5) and −5% (RCP 8.5) in FF. Without CO₂ fertilization (constant 380 ppm), SOC losses were twice as large: −5% (RCP 2.6), −6% (RCP 4.5), and −13% (RCP 8.5) in FF. Extreme indices showed NHD increasing by 160% under RCP 8.5 in FF (from 36 to 93 days), and WSDI increasing from 8 days (H) to 90 days (RCP 8.5, FF). Correlations between extreme indices and modeled variables intensified under RCP 8.5, with CO₂ fertilization mitigating negative impacts of temperature extremes on productivity.
**Clinical Implications:** The study demonstrates that while climate change—particularly CO₂ fertilization—may boost grassland productivity and milk yields, it simultaneously drives SOC losses, especially under high-emission scenarios. Maintaining productivity requires substantially higher nitrogen fertilizer inputs (e.g., +53% under RCP 8.5 in FF), which carries environmental costs (leaching, N₂O emissions). Under RCP 8.5, extreme heat and drought may render some years unsuitable for milk production. The findings underscore a fundamental trade-off: targeting productivity likely accelerates soil carbon loss, and SOC stocks can only be increased through management changes that reduce carbon exports (e.g., grazing intensity, harvest frequency). For clinicians and agricultural policymakers, these results highlight the need for adaptive management strategies that balance food production with soil carbon conservation, particularly as extreme events become more frequent.