mixed Rossby-gravity waves 混合Rossby重力波
gravity waves 重力波
ducted gravity waves 受导重力波
linear gravity waves 线性重力波
guided gravity waves 受导重力波
inertia gravity waves 重力惯性波
inertia-gravity waves 惯性重力波
inertial gravity waves 惯性重力波
The emission of inertia-gravity waves from the adjustment of balanced flows(or,basically,vortical flows) is currently regarded as a new mechanism of the production of inertia-gravity waves and referred as the spontaneous emission.
平衡流(或粗略地说涡旋流)调整目前被认为是惯性重力波产生的一种新的机制并被称为自发辐射问题。
参考来源 - 涡旋流自发辐射惯性重力波的初步解析研究By means of numerical and analytic methods and FEM method the gravity waves generated by the high-frequency external excitation in the liquid-elastic shell coupled system were ulteriorly researched, the reasoning of the emergence of the waves were well explained.
通过数值方法、解析方法及有限元分析对弹性壳液耦合系统受高频激励液面所出现的低频大幅重力波的现象进行的研究,解释了低频大幅重力波的产生机理。
参考来源 - 矩形壳液耦合系统低频大幅波的分析·2,447,543篇论文数据，部分数据来源于NoteExpress
The pattern is of atmospheric gravity waves playing on the surface of the ocean.
这张图案是在大气重力波对海洋表面所产生的影响。
Normal swells, known technically as gravity waves, are created by wind pushing the surface of the sea up and gravity then pulling it down, causing it to bounce.
一般的波浪，技术上被成为重力波，是由于风推动着海洋表面上升而后又在重力的作用下被拉向下方，这便会导致海水的回弹。
Atmospheric gravity waves form when buoyancy pushes air up, and gravity pulls it back down.
当浮力把空气向上推，而重力又把它向下拉的时候，就会形成大气的重力波。
应用推荐