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Updated: Jul 2, 2025

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由Argo-O2,神经网络和反向计算揭示的人类碳通道向北大西洋内部
Rémy Asselot1, Lidia I Carracedo2, Virginie Thierry2
1University of Brest, Ifremer, CNRS, IRD, Laboratory of Spatial and Physical Oceanography (LOPS), 29280, Plouzané, France. remy.asselot@ifremer.fr.
Nature communications
|February 22, 2024
概括
在亚极北大西洋中人类产生的二氧化碳储存得到了澄清. 阿戈-O2浮标揭示了由水质转换和深冬对流驱动的 CO2 逐步加深,增强了对海洋碳吸收的理解.
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:
- 亚极北大西洋 (SPNA) 对于人为二氧化碳 (Cant) 储存至关重要.
- 坎特分布已知,但其进入海洋内部的途径尚不清楚.
研究的目的:
- 在SPNA中沿浮动路径确定坎特演变,使用准拉格朗的方法.
- 为了研究水质转换在坎特透中的作用.
主要方法:
- 在SPNA中利用了三个Argo-O2浮标 (2013-2018) 的观测结果.
- 采用现有的神经网络和反向计算技术.
- 分析了坎特分布和混合过程.
主要成果:
- 坎特在SPNA中沿着浮动轨迹逐步加深.
- 亚极模式 水的形成使冰岛盆地的冬季混合层中的Cant同质化.
- 在伊明格和拉布拉多盆地的深冬对流将Cant混合到1400和1800dbar,稀释峰值度.
结论:
- 水质转化是坎特透到海洋内部的主要机制.
- 阿戈-O2的观测,加上其他方法,提供可靠的坎特估计.
- 这种方法使海洋Cant含量的高分辨率研究成为可能.
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