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在深层溢流的体积运输的变化,在南方10度上,在东九度山脊上
Shanwu Zhang1,2, Fuwen Qiu3,4, Hangyu Chen1,2
1Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, 361005, China.
Scientific reports
|July 11, 2025
概括
深海溢出对于印度洋循环至关重要. 这项研究量化了溢流量,并揭示了风驱动的变性,突出了罗斯比波在深流调节中的作用.
科学领域:
- 海洋学 海洋学 海洋学
- 物理海洋学 物理海洋学
- 气候科学 气候科学
背景情况:
- 跨越九东山脊的深度溢出对印度洋南部翻转循环至关重要.
- 这些深层溢流的精确体积运输和时间变化仍然不太清楚.
研究的目的:
- 为了量化深层溢出的体积运输量,在Nineetyeast山脊上的子上.
- 调查这些溢出的时间变化,并确定驱动机制.
主要方法:
- 利用17个月的速度概况记录来估计体积运输.
- 在数值模型输出上使用光谱实证直角函数分解和光线跟踪.
- 分析了溢出变化和风力应力曲线之间的相关性.
主要成果:
- 估计的时间平均体积运输的溢出附近10°S在1.3 Sv (0.8-1.6 Sv在95%的信心).
- 在溢出运输中观察到显著的半年 (170天) 和季内 (73天) 变化.
- 证明了溢出变化和风力应力曲线在九九东山脊以东之间存在强烈的相关性.
结论:
- 深度溢出是印度洋循环的重要组成部分,运输量与理论估计相比.
- 通过罗斯比波,风驱动的变化在调节印度洋东南部的深流和溢流方面发挥着至关重要的作用.
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