有机碳的海洋物理注射
Marco Bellacicco1, Salvatore Marullo2, Giorgio Dall'Olmo3
1Istituto di Scienze Marine, Consiglio Nazionale delle Ricerche, Roma, Italy. marco.bellacicco@cnr.it.
Nature communications
|August 2, 2025
概括
物理注入 (PIP) 通过混合和吸附出口大量的海洋碳,而不仅仅是沉没物质. 这项研究量化了PIP.
科学领域:
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
- 气候科学 气候科学
背景情况:
- 传统的海洋碳出口估计侧重于沉没颗粒和迁徙生物.
- 对于碳出口,越来越多地认识到诸如上海混合和向导之类的动态途径.
- 对这些动态路径的全球性,基于观察的估计仍然很少.
研究的目的:
- 量化由物理注入 (PIP) 驱动的碳出口.
- 评估PIP驱动的碳出口的跨年变化.
- 为了估计与PIP出口流程相关的不确定性.
主要方法:
- 利用4D数据驱动的时间序列 (1997-2018) 对微粒有机碳 (POC) 和海洋循环.
- 嵌入了溶解有机碳 (DOC) 的3D气候学场.
- 分析了作为关键出口机制的垂直扩散,引进和引向.
主要成果:
- 在POC出口估计中,垂直扩散是占主导地位的,但也是最不确定的过程.
- 在最大扩散性假设下,估计POC出口为0.37 Pg C yr-1和DOC出口为0.48 Pg C yr-1.
- 培训和宣传贡献与POC年度周期和上层混合密切相关.
结论:
- 物理注入在海洋碳出口中起着至关重要的作用,加上生物生产和混合.
- PIP出口的年间变化与ENSO和SAM指数相关,特别是在南洋.
- 这些发现突显了PIP动态与南大洋中介/模式水形成之间的联系.
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