首页|基于哨兵一号SAR成像的南奥克尼海台内孤立波研究

基于哨兵一号SAR成像的南奥克尼海台内孤立波研究

扫码查看
大量来自哨兵一号卫星的合成孔径雷达(Synthetic aperture radar,SAR)成像产品揭示了南奥克尼海台南侧是一处内孤立波生成的热点区域,该区域内孤立波的空间分布和特征参数首次被揭示.统计结果显示该区域内孤立波具有两种传播方向:一类向南往深海传播,另一类向东沿等深线传播.此外,观测到的内孤立波波长平均值为300 m,波峰长度平均值为80 km,简单的统计分析显示遥感观测到的内孤立波绝大多数在大潮前后生成.经过计算研究区域内的正压潮力得出南奥克尼海台南侧45°W的1 000 m等深线是一处理想的内潮生成源,通过回溯内孤立波的生成时刻得出东向传播的内孤立波属于典型的内潮释放机制.最后,本研究结合两层的Benjamin-Ono方程和遥感观测结果对内孤立波的振幅和相速度进行了反演,反演得到内孤立波振幅约为9 m,传播相速度约为0.5 m/s.
Sentinel-1 SAR Observation of Internal Solitary Waves Generated at the South Orkney Plateau
A lot of Sentinel-1A/B synthetic aperture radar(SAR)observation taken from South Orkney Islands indicate that its southern plateau can be an oceanic hot spot for internal solitary waves(ISWs).The spatial distribution and physical parameters of these waves are disclosed for the first time.The statistical results show that observed ISWs have two main propagation paths towards south and east off the generation site and that they have an average wavelength of 300 m and crestlength around 80 km.Besides,most observed ISWs are generated before and after local spring tide.The barotropic body force is calculated to identify potential internal tides(ITs)generation locations.It is found that the 1 000 iso-baths near 45°W can be an ideal internal tide generation site.We also calculate the generation time for eastward propagating ISWs at ideal internal tide generation site which validates the internal tide release mechanism.It shows the waves are form just to the west of the sill at the time of maximum westward flow and disintegrate into strong ISWs when westward tidal current slackens.Finally,we use the Benja-min-Ono equation in a two-layer mechanism to simulate the characteristic parameters of the studied ISWs.The derived wave amplitude and phase speed are around 9 m and 0.5 m/s respectively,but we lack in situ observation to verify.

internal solitary wavessynthetic aperture radar(SAR)South Orkney PlateauWeddell Sea

刘海涛、王彩霞

展开 >

中国海洋大学海洋与大气学院 物理海洋教育部重点实验室,山东青岛 266100

内孤立波 合成孔径雷达 南奥克尼海台 威德尔海

2025

中国海洋大学学报(自然科学版)
中国海洋大学

中国海洋大学学报(自然科学版)

北大核心
影响因子:0.474
ISSN:1672-5174
年,卷(期):2025.55(2)