微弱的北方和强大的热带土地碳吸收来自大气二氧化碳的垂直配置
Britton B Stephens1, Kevin R Gurney, Pieter P Tans
1National Center for Atmospheric Research, Boulder, CO 80305, USA. stephens@ucar.edu
概括
大气中的二氧化碳 (CO2) 测量挑战模型,表明北方碳吸收较弱,热带碳汇可能较强. 这表明北方陆地吸收工业二氧化碳排放的作用比以前认为的要小.
科学领域:
- 大气化学和碳循环科学.
背景情况:
- 大气模型传统上估计了从热带到北度的陆地碳转移.
- 以前的估计表明,北方的碳吸收和热带碳排放量相当大.
研究的目的:
- 通过比较它们的二氧化碳转移估计值与观察到的垂直大气二氧化碳分布来调查大气模型的准确性.
- 重新评估热带和北方生态系统在全球碳循环中的作用.
主要方法:
- 分析中午垂直大气二氧化碳 (CO2) 的分布.
- 观察到的二氧化碳梯度与来自多个大气模型的输出进行比较.
- 对热带和北方地区的碳流量估计进行了改进.
主要成果:
- 观察到的年均垂直二氧化碳梯度与预测大规模热带到北方碳转移的模型不一致.
- 最好复制观察到的梯度的模型估计较弱的北方碳吸收 (-1.5 Pg C年(-1)) 和较弱的热带排放 (+0.1 Pg C年(-1)).
- 这些修订后的估计与先前的共识数据有很大差异 (-2.4 Pg C年(-1) 吸收, +1.8 Pg C年(-1) 排放).
结论:
- 北部陆地吸收工业二氧化碳排放的作用似乎比以前估计的要小.
- 在考虑土地使用排放后,热带生态系统可以作为重要的碳汇.
- 修改大气二氧化碳运输模型对于准确了解全球碳动态至关重要.
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