低压风暴导致南大洋的氧化排放
Colette L Kelly1, Bonnie X Chang2, Andrea F Emmanuelli3,4
1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, USA. colette.kelly@whoi.edu.
Nature communications
|January 26, 2026
概括
强大的温室气体氧化的海洋排放难以衡量. 新的机器学习方法揭示了南洋风暴显著增加了这些排放,影响了全球温室气体预算.
科学领域:
- 海洋学 海洋学 海洋学
- 大气化学 大气化学
- 气候科学 气候科学
背景情况:
- 氧化 (N2O) 是一个重要的温室气体和破坏臭氧层的物质.
- 海洋N2O排放很难量化,因为它具有很高的时空变化.
- 南洋是空海气交换的关键区域,受到旋风风暴的影响.
研究的目的:
- 为了量化南大洋的氧化排放量,考虑到风暴的影响.
- 改进对海洋在全球N2O预算中的作用的估计.
- 为海洋生物地化学研究利用新型数据源.
主要方法:
- 机器学习算法应用于生物地球化学Argo浮动数据.
- N2O度和空气-海梯度是从漂浮物观测中得出的.
- 分析了低压风暴系统对N2O流量的影响.
主要成果:
- 机器学习成功地从Argo浮标中获得了N2O观测结果.
- 低压风暴被确定为N2O排放的热点.
- 考虑到风暴,估计每年南洋N2O流量增加了88%.
结论:
- 南洋对全球N2O排放的贡献比以前估计的要大.
- 暴风雨显著增加了空海N2O梯度和排放.
- 南大洋可能是温室气体的沉积槽比以前所认为的要弱.
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