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Atmospheric water vapor and soil moisture jointly determine the spatiotemporal variations of CO2 fluxes and evapotranspiration across the Qinghai-Tibetan Plateau grasslands

EngineeringTerrestrial EcosystemAtmospheric Water VaporDrylandsTerrestrial Ecosystem ProductivityCo2 FluxesSoil MoistureEarth ScienceTibetan PlateauClimate Change