Using discrete air
sampling, atmospheric CO2 and its stable carbon (d13C) and oxygen (d18O) isotopic ratios have been measured since 1994 in a
cool-temperate deciduous forest in central Japan influenced strongly by the
Asian monsoon. In this paper, the results are shown and the temporal variations
on different time scales are discussed.
Author: S. Murayama, N. Saigusa, S. Yamamoto, C. Takamura, et al (s dot murayama at aist dot go dot jp)
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