Seasonal and inter-annual variations in CO2 fluxes over 10 years in an alpine shrubland on the Qinghai-Tibetan Plateau, China
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The alpine shrubland acts as weak CO2 sink with −74.4 ± 12.7 g C m−2 year−1 (Mean ± S.E.).

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Thermal conditions (GDD and GSL) regulated variations of annual GPP.

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Water status during vegetation onset played important role in variations of annual RES.

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ANPP of nested-grass accounted for variations of annual shurbland NEE.

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