ocean internal waves 海洋内波
near inertial internal waves 近惯性内波
near-inertial internal waves 近惯性内波
shallow water internal waves 浅水内波
Equator ocean internal waves 赤道大洋内波
In-situ measurements and remote sensing have showed that internal waves are ubiquitous in the ocean. It is one of the main mechanisms of tidal energy dissipation and ocean mixing.
现场与遥感观测都表明,海洋内波广泛分布于世界各个海区,它是潮汐能耗散和海洋内部混合的主要机制之一。
参考来源 - 海洋内波的遥感与数值模拟研究The internal waves can propagate along the level direction and the perpendicularity one.
内波不仅可以沿着水平方向传播,而且还具有垂向传播的特性。
参考来源 - 粘性分层流中水下航行体尾迹在随机海面中的表现特征研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The generation mechanism of orientating sedimentary structure is very important to the recognition of the internal-waves sediments.
明确指向沉积构造的形成机理对于内波沉积的识别具有重要意义。
Internal waves happen because the ocean is layered. Deep water is cold, dense, and salty, while shallower water is warmer, lighter, and fresher.
出现内波是因为海洋是分层的，深层水更凉，密度高而且含盐量高，浅层水更暖和，密度小而且更淡。
This image shows both internal waves and surface waves on the Indian Ocean near the Andaman Islands.
这张图片显示了印度洋安达曼群岛附近的内波和表面流。
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