直接的观察证据表明,南大洋的二氧化碳吸收很大
Yuanxu Dong1,2, Dorothee C E Bakker1, Thomas G Bell2
1Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, UK.
Science advances
|July 24, 2024
概括
南大洋吸收的二氧化碳 (CO2) 比以前估计的要多25%. 考虑海洋温度和更高的数据分辨率是理解这一重要气候调节的关键.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 南大洋对于吸收人为二氧化碳 (CO2) 是至关重要的.
- 目前该地区的二氧化碳流量估计存在重大不确定性,缺乏直接验证.
- 准确的流量估计对于气候建模和了解地球碳循环至关重要.
研究的目的:
- 通过直接测量重新评估南洋二氧化碳吸收.
- 确定现有的二氧化碳流量估计中的差异原因.
- 为了提高未来二氧化碳流量计算的准确性.
主要方法:
- 利用了七个独立的,直接测量的空海二氧化碳流量数据集.
- 分析了上海温度梯度对流量估计的影响.
- 评估了流量产品中时间分辨率的影响.
- 将直接测量与基于船上数据集的估计,浮动数据和生物地质化学模型进行了比较.
主要成果:
- 与船上的估计相比,直接测量表明南大洋的二氧化碳吸收量比船上的估计高25%.
- 上部海洋温度梯度和时间分辨率显著影响流量计算.
- 气体转移速度的参数化不是流量异常的主要原因.
- 分析浮动数据和模型低估了观察到的二氧化碳吸收,可能错过了小规模的高流量事件.
结论:
- 南大洋的二氧化碳吸收可能被严重低估.
- 结合温度校正和更高的时间分辨率对于准确的流量估计至关重要.
- 未来的研究应该专注于在模型中表示小规模的高流量事件.
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