Graduate School of Environmental Science, Hokkaido University, Sapporo, Japan.
Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan.
Sci Rep. 2020 Jun 1;10(1):8838. doi: 10.1038/s41598-020-65661-2.
The oceanic external nitrogen (N) deposition to the global ocean is expected to rise significantly owing to human activities. The Southern Ocean (SO) is an important pathway, which brings external influences into the ocean interior. It touches the borders of several developing countries that emit a large amount of anthropogenic nitrogen. To comprehend the dynamics of N in the SO, we developed a new method to assess the change in the oceanic uptake of N (ΔN) in the entire SO. We obtained the spatiotemporal distribution of ΔN in the SO by applying this method to a high-resolution grid data constructed using ship-based observations. During the 1990s to the 2010s, N increased significantly by 67 ± 1 Tg-N year in the SO. By comparing this value with the rate of N deposition to the ocean, the SO has received ~70% of N deposition to the global ocean, indicating that it is the largest uptake region of anthropogenic nitrogen into the ocean interior.
由于人类活动,海洋的外部氮(N)沉积预计将大幅增加。南大洋(SO)是一个重要的途径,它将外部影响带入海洋内部。它与几个排放大量人为氮的发展中国家接壤。为了了解 SO 中 N 的动态,我们开发了一种新方法来评估整个 SO 中海洋 N 吸收的变化(ΔN)。我们通过将该方法应用于使用船载观测构建的高分辨率网格数据,获得了 SO 中ΔN 的时空分布。在 1990 年代至 2010 年代期间,SO 中的 N 显著增加了 67±1Tg-N 年。通过将此值与海洋 N 沉积的速率进行比较,SO 接收了全球海洋 N 沉积的约 70%,表明它是人为氮进入海洋内部的最大吸收区域。