概括
在赤道印度洋的海洋流被大型垂直尺度和赤道被困运动所主导. 接近地表的循环直接响应风的变化,在季风之间形成东向喷气.
科学领域:
- 海洋学 海洋学 海洋学
- 流体动力学 流体动力学
- 气象学 天气学
背景情况:
- 1976年之前的研究表明,赤道印度洋的大型垂直尺度上的能量变化.
- 了解赤道海洋动态对于气候和天气模式预测至关重要.
研究的目的:
- 调查印度洋西部赤道水平流的详细垂直概况.
- 分析海洋变化的能量主导和空间尺度.
- 检查近地平线环流和风场变化之间的关系.
主要方法:
- 在1979年春夏期间,从索马里海岸到62°E的赤道印度洋进行测量.
- 使用水平电流的详细垂直配置文件.
- 使用卫星追踪的漂流浮标来追踪地表电流.
主要成果:
- 能量变化是由几百米的垂直尺度主导的,仅限于赤道附近.
- 接近地表的赤道循环显示了对风场变化的直接反应.
- 一个突出的东方赤道表面喷射被观察到,跨越海洋的宽度.
- 区域速度波动在整个观测区域显示出一致的模式.
结论:
- 赤道印度洋的速度场在很大程度上受到长期的影响,赤道上被困的运动具有广泛的区域尺度.
- 东流是由东风在东北和西南季风之间产生的.
- 变量尺度表明该地区的动态状态持续存在.
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