“…For very low SWC (<0.04 m 3 m −3 ), NEE increased with PAR at first and then decreased considerably (NEE gets more positive resulted from ecosystem loss carbon to the atmosphere) when PAR exceeded 1300 µmol photons m −2 s −1 . A reduction in NEE in dry conditions has been observed in different ecosystems (Sims and Bradford, 2001;Hastings et al, 2005;Li et al, 2005;Fu et al, 2006;Aires et al, 2008b;Holst et al, 2008;Wang et al, 2008) and caused by midday stomata closure when irradiance, temperature, and VPD are all high, when the SWC is low (Sims and Bradford, 2001;Li et al, 2005;Aires et al, 2008b) or by enhanced ecosystem respiration at high temperature (Fu et al, 2006;Holst et al, 2008).…”