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
These waves, internal waves, can be tens of kilometers long and can last several hours.
这些波浪，内波，可能会有几万米长，持续几个小时。
Internal solitary waves are a kind of special internal waves, which could bring enormous energy and propagate long distance in the ocean with its wave form basically unchanged.
海洋内孤立波是一种携带巨大能量的特殊内波，它能够在海洋中长距离传播而保持波形基本不变。
Most of the internal waves travel westly.
内波传播方向以西向为主。
应用推荐