相关实验视频
Updated: Jul 11, 2026

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
概括
在夏威夷的东北发现了 mesoscale baroclinic eddies,它们在大规模海洋流的影响下向西漂移. 这项研究证实了它们在太平洋的存在.
科学领域:
- 海洋学 海洋学 海洋学
- 流体动力学 流体动力学
- 地质物理学 地质物理学
背景情况:
- 来自太平洋贸易风地区的地表温度数据显示,与平均状态的差异很大.
- 这些扰动的区域波长大约为480公里.
研究的目的:
- 为了识别和描述太平洋中大尺度巴洛克林尼克旋.
- 为了确定这些旋的漂移速度,并调查大规模电流对它们运动的影响.
主要方法:
- 对地下温度测量的分析.
- 计算旋漂移速度并与大规模的巴洛克林尼克流量进行比较.
主要成果:
- 测量尺度的巴罗临床旋被确定为以4.7 +/- 2.0cm/s的速度向西漂移.
- 在200米深 (1.5 +/- 0.7厘米/秒向西) 的大型巴洛克林尼克流量与流漂移速度相当.
- 这表明大规模流量对流运动的显著影响.
结论:
- 证实了太平洋中等层次旋的存在.
- 厄迪漂移受到周围大规模海洋流动的强烈影响.
- 这些发现扩大了对太平洋海洋动态的了解.
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