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- W2359150934 abstract "Using the CO2 flux data obtained by the eddy covariance method in the northeast of the Qinghai-Tibetan Plateau in 2005,we analyzed the carbon dynamics in relation to the meteorological factors.The results showed that the alpine wetland ecosystem was a carbon source,and emitted 316.02gCO2·m-2 to the atmosphere in 2005 with 230.16 gCO2·m-2 absorbed in the growing season from May to September and 546.18 gCO2·m-2 released in the non-growing season from January to April and from October to December.The maximum of the averaged daily CO2 uptake rates and release rates was(0.45±0.0012) mgCO2·m-2·s-1(Mean SE) in July,and(0.22±0.0090) mgCO2·m-2·s-1 in August respectively.The averaged diurnal variation showed a single-peaked pattern in the growing season but exhibited very small fluctuation in the non-growing season.Net ecosystem exchange(NEE) and gross primary production(GPP) were all correlated with some meteorological factors,and showed a negative linear correlation with aboveground biomass,while a positive correlation existed between the ecosystem respiration(Res)and those factors." @default.
- W2359150934 created "2016-06-24" @default.
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- W2359150934 date "2008-01-01" @default.
- W2359150934 modified "2023-09-24" @default.
- W2359150934 title "CO_2 flux in alpine wetland ecosystem on the Qinghai-Tibetan Plateau" @default.
- W2359150934 hasPublicationYear "2008" @default.
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