在莫桑比克海峡中介尺度旋的特征
Linfei Bai1,2,3, Guohao Zhu2, Haojie Huang2
1Jiangsu Key Laboratory of Marine Bioresources and Environment /Jiangsu Key Laboratory of Marine Bio-technology, Jiangsu Ocean University, Lianyungang, Jiangsu Province, China.
PloS one
|April 29, 2024
概括
在莫桑比克海峡中使用卫星数据分析了 mesoscale . 反气旋旋更加普遍和更大,受当地风的影响,影响海面温度.
科学领域:
- 海洋学 海洋学 海洋学
- 流体动力学 流体动力学
- 卫星遥感 卫星遥感 卫星遥感
背景情况:
- 莫桑比克热流在区域海洋动态中起着至关重要的作用.
- 中等尺度的旋显著影响海洋流中的热量和动量传输.
- 了解的特征对于气候和生态研究至关重要.
研究的目的:
- 为了研究莫桑比克海峡中层层旋的特征.
- 为了确定旋生成的热点,并分析旋的特性.
- 探索风力强迫和波波动对海面温度的影响.
主要方法:
- 利用了从2010年到2019年的卫星高度测量数据.
- 采用了探测和跟踪算法.
- 分析了风应力,的动能和海面温度之间的相关性.
主要成果:
- 在莫桑比克海峡确定了1,086个中级旋风 (509个旋风,577个反旋风).
- 马达加斯加西北部海岸被确定为主要的旋生成热点.
- 反旋风旋的平均幅度 (24.23厘米) 和半径 (82.7公里) 比旋风旋更大.
- 当地风力强迫,特别是季风和贸易风,显著影响了的形成和的动能分布.
- 埃迪的变异性显示出与季节性海面温度异常的潜在联系.
结论:
- 中级,特别是反气旋,是莫桑比克海峡的突出特征.
- 风力强迫是这个地区 generation和特征的关键驱动因素.
- 动力学可能在调节当地的海面温度方面发挥着重要作用.
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