期刊
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
卷 60, 期 2, 页码 213-225出版社
TAYLOR & FRANCIS LTD
DOI: 10.1111/j.1600-0889.2007.00334.x
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We present measurements of atmospheric O-2/N-2 and CO2 mixing ratios taken at Hateruma Island (HAT) and Cape Ochi-Ishi (COI) in Japan. Global carbon sinks are estimated from the tracer atmospheric potential oxygen (APO) calculated as the weighted sums of the observed O-2/N-2 and CO2, and the global CO2 data from the NOAA/ESRL GMD flask sampling network. The oceanic and land biotic sinks are 2.4 +/- 0.7 and 0.5 +/- 0.9 Pg C yr(-1), respectively, for the 7-yr period (July 1998-July 2005) and 2.1 +/- 0.7 and 1.0 +/- 0.9 Pg C yr(-1), respectively, for the 6-yr period (July 1999-July 2005). The former 7-yr estimates are based on the data from HAT only, while the latter 6-yr estimates are obtained using data from both HAT and COI. These estimations include an ocean outgassing correction of 0.48 Pg C yr(-1). The instantaneous rates of change in the APO trends show large interannual variability with peak-to-peak amplitudes of about 30 per meg yr(-1). The winter anomalies in the APO trend are the major contributor to the interannual variability, and the oceanic O-2 influx associated with winter ventilation may be a significant cause of the variability in APO.
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