Dynamics of the Indian-Ocean oxygen minimum zones
Progress in Oceanography(2013)
摘要
•The main oxygen source for the northern Indian Ocean is Southern-Hemisphere water.•Advection and vertical eddy mixing shift the ASOMZ to the central/eastern basin.•The BBOMZ is weaker because there is less detritus along the western boundary.•The OMZs lack a prominent annual cycle because remineralization is a slow process.
更多查看译文
AI 理解论文
溯源树
样例
![](https://originalfileserver.aminer.cn/sys/aminer/pubs/mrt_preview.jpeg)
生成溯源树,研究论文发展脉络
Chat Paper
正在生成论文摘要