全球碳沉积点及其从大气O2和delta13C中推断出的可变性
M Battle1, M L Bender, P P Tans
1Department of Geoscience, Guyot Hall, Princeton University, Princeton, NJ 08544 USA.
概括
大气中的氧气 (O2) 测量显示,陆地和海洋在1991-1997年间吸收了大量的碳. 这与20世纪80年代形成鲜明对比,表明地球系统的碳吸收是可变的.
科学领域:
- 地球系统科学 地球系统科学
- 大气化学 大气化学
- 海洋学 海洋学 海洋学
背景情况:
- 大气中的O2和二氧化碳 (CO2) 水平受到全球碳循环过程的影响.
- 上世纪80年代之前的估计表明,几乎中性陆地生物圈碳平衡.
研究的目的:
- 通过大气O2测量量,量化陆地生物圈和海洋的碳捕获量.
- 将当代碳吸收与历史数据和同位素流量估计进行比较.
主要方法:
- 对大气O2度的时间序列测量的分析.
- 将O2数据与delta13CO2 (一种碳同位素比率) 的测量进行比较.
- 将同位素流量数据与大气测量的整合.
主要成果:
- 在1991年中期至1997年中期期间,陆地生物圈每年排放了1.4 +/- 0.8 GtC,海洋2.0 +/- 0.6 GtC/年.
- 这一时期显示出陆地生物圈的快速碳储存,与20世纪80年代几乎中性平衡不同.
- 同位素流量估计与O2衍生的流量一致,表明可变的碳吸收.
结论:
- 大气中的O2和delta13C数据提供了一个强有力的信号,表明全球碳储存的跨年变化.
- 陆地生物圈和海洋都表现出动态和可变的碳吸收.
- 这些发现凸显了地球碳汇对环境变化的敏感性.
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