全球范围的随机底压波动来自海洋内在的变化.
Mengnan Zhao1, Rui M Ponte1, Thierry Penduff2
1Atmospheric and Environmental Research Inc., Lexington, MA, USA.
Science advances
|July 21, 2023
概括
海洋底压力变化受到海洋内在过程的影响. 一种新发现的海洋底压力变化的全球模式是由德雷克海峡附近的局部动力驱动的.
科学领域:
- 海洋学 海洋学 海洋学
- 流体动力学 流体动力学
- 气候科学 气候科学
背景情况:
- 海洋内在的过程,如中等层流,显著影响海洋底部压力 (pb) 的变化.
- 这些过程可以通过反向能量级联或巴洛克林尼克不稳定性在更大的规模上产生变化.
研究的目的:
- 为了识别和描述海洋底部压力波动的全球范围内在模式.
- 在每月的时间表上阐明驱动这种模式的潜在机制.
主要方法:
- 对海洋学模型输出的分析.
- 研究内在变化模式的研究.
- 检查旋驱动的动力学和巴罗热波传播.
主要成果:
- 确定了月度时间尺度上海洋底压力变化的全球范围内在模式.
- 这种模式在德雷克海峡附近显示最大幅度,南大洋和大西洋/北极洋之间的极性相反.
- 该机制涉及德雷克通道附近局部的旋驱动的pb异常,通过巴罗热波传播.
结论:
- 发现了一种新的海洋底压力变化的全球内在模式.
- 这种模式是由局部的动力学和随后的巴罗热波波调整驱动的.
- 这些发现与观察到的海洋底压力变化模式一致.
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