在空中观测中明显的南大洋碳吸收
Matthew C Long1, Britton B Stephens1, Kathryn McKain2,3
1National Center for Atmospheric Research, Boulder, CO, USA.
概括
南洋的二氧化碳 (CO2) 吸收对气候调节至关重要. 这项研究使用大气二氧化碳测量估计每年净二氧化碳吸收量为0.53,完善了气候模型.
科学领域:
- 地球系统科学
- 大气化学
- 海洋学
背景情况:
- 南洋对全球大气中的二氧化碳 (CO2) 水平有很大影响.
- 目前对该地区的空气和海洋二氧化碳交换的估计显示出相当大的差异.
研究的目的:
- 通过大气二氧化碳梯度来限制南洋的空气-海洋二氧化碳交换.
- 提供南大洋二氧化碳净流量的更准确的估计.
主要方法:
- 利用大气运输模型将二氧化碳流与水平和垂直的二氧化碳梯度联系起来.
- 应用在飞机上的空气二氧化碳垂直梯度测量流量限制.
- 2009年至2018年期间南方45°S的估计年平均CO2流量.
主要成果:
- 估计每年南洋二氧化碳的平均流量为0.53±0.23克 (净吸收量).
- 结果与大气逆转估计和海洋表面的PCO2产物一致.
- 比一些最近的浮动数据解释所表明的更强的年平均二氧化碳吸收.
结论:
- 基于飞机的二氧化碳梯度测量为南洋空海二氧化碳流提供了强大的约束.
- 这项研究改进了南大洋碳捕获的估计.
- 这些发现有助于更好地了解海洋在全球碳循环中的作用.
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