Consequently, the simulated NEP exhibited a decreasing trend under a warming climate.
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Projected changes of alpine grassland carbon dynamics in response to climate change and elevated CO2 concentrations under Representative Concentration Pathways (RCP) scenarios.
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With respect to the response to the decadal change of precipitation, the dynamics of the ΔNPP and ΔRh showed an increasing trend with ΔPrecipitation, while these positive responses tended to be stagnant ( Fig 5A and 5B ).