2004Journal of Geophysical Research AtmospheresOpen access

Seasonal patterns of gross primary production and ecosystem respiration in an alpine meadow ecosystem on the Qinghai‐Tibetan Plateau

Tomomichi Kato, Yanhong Tang, Song Gu, Mitsuru Hirota, Xiaoyong Cui, Mingyuan Du, Yingnian Li, Xinquan Zhao, Takehisa Oikawa

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Abstract

We measured the net ecosystem CO 2 exchange (NEE) in an alpine meadow ecosystem (latitude 37°29′–45′N, longitude 101°12′–23′E, 3250 m above sea level) on the Qinghai‐Tibetan Plateau throughout 2002 by the eddy covariance method to examine the carbon dynamics and budget on this unique plateau. Diurnal changes in gross primary production (GPP) and ecosystem respiration (R e ) showed that an afternoon increase of NEE was highly associated with an increase of R e . Seasonal changes in GPP corresponded well to changes in the leaf area index and daily photosynthetic photon flux density. The ratio of GPP/R e was high and reached about 2.0 during the peak growing season, which indicates that mainly autotrophic respiration controlled the carbon dynamics of the ecosystem. Seasonal changes in mean GPP and R e showed compensatory behavior as reported for temperate and Mediterranean ecosystems, but those of GPP max and R emax were poorly synchronized. The alpine ecosystem exhibited lower GPP (575 g C m −2 y −1 ) than, but net ecosystem production (78.5 g C m −2 y −1 ) similar to, that of subalpine forest ecosystems. The results suggest that the alpine meadow behaved as a CO 2 sink during the 1‐year measurement period but apparently sequestered a rather small amount of C in comparison with similar alpine ecosystems.

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We measured the net ecosystem CO 2 exchange (NEE) in an alpine meadow ecosystem (latitude 37°29′–45′N, longitude 101°12′–23′E, 3250 m above sea level) on the Qinghai‐Tibetan Plateau throughout 2002 by the eddy covariance method to examine the carbon dynamics and budget on this unique plateau. Diurnal changes in gross primary production (GPP) and ecosystem respiration (R e ) showed that an afternoon increase of NEE was highly associated with an increase of R e . Seasonal changes in GPP corresponded well to changes in the leaf area index and daily photosynthetic photon flux density. The ratio of GPP/R e was high and reached about 2.0 during the peak growing season, which indicates that mainly autotrophic respiration controlled the carbon dynamics of the ecosystem. Seasonal changes in mean GPP and R e showed compensatory behavior as reported for temperate and Mediterranean ecosystems, but those of GPP max and R emax were poorly synchronized. The alpine ecosystem exhibited lower GPP (575 g C m −2 y −1 ) than, but net ecosystem production (78.5 g C m −2 y −1 ) similar to, that of subalpine forest ecosystems. The results suggest that the alpine meadow behaved as a CO 2 sink during the 1‐year measurement period but apparently sequestered a rather small amount of C in comparison with similar alpine ecosystems.

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Available abstract

We measured the net ecosystem CO 2 exchange (NEE) in an alpine meadow ecosystem (latitude 37°29′–45′N, longitude 101°12′–23′E, 3250 m above sea level) on the Qinghai‐Tibetan Plateau throughout 2002 by the eddy covariance method to examine the carbon dynamics and budget on this unique plateau. Diurnal changes in gross primary production (GPP) and ecosystem respiration (R e ) showed that an afternoon increase of NEE was highly associated with an increase of R e . Seasonal changes in GPP corresponded well to changes in the leaf area index and daily photosynthetic photon flux density. The ratio of GPP/R e was high and reached about 2.0 during the peak growing season, which indicates that mainly autotrophic respiration controlled the carbon dynamics of the ecosystem. Seasonal changes in mean GPP and R e showed compensatory behavior as reported for temperate and Mediterranean ecosystems, but those of GPP max and R emax were poorly synchronized. The alpine ecosystem exhibited lower GPP (575 g C m −2 y −1 ) than, but net ecosystem production (78.5 g C m −2 y −1 ) similar to, that of subalpine forest ecosystems. The results suggest that the alpine meadow behaved as a CO 2 sink during the 1‐year measurement period but apparently sequestered a rather small amount of C in comparison with similar alpine ecosystems.

Key concepts: Ecosystem respiration, Primary production, Eddy covariance, Ecosystem, Environmental science, Atmospheric sciences, Terrestrial ecosystem, Plateau (mathematics)

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