| 1. | The most easily observed example of such gravity waves is that of waves in the lee of mountains .
最容易观测到的这种重力波是产生在山背冈的重力波。 |
| 2. | The jet stream and gravity wave in the atmosphere
高空急流与重力内波 |
| 3. | Capillary gravity wave
毛细重力波 |
| 4. | Mechanism of low - frequency large - amplitude gravity waves of liquid in cylindrical shell container
圆柱形弹性壳液耦合系统大幅低频重力波振动机理的研究 |
| 5. | Numerical simulations of mountain gravity waves generated by multi - layer flow over an isolated mountain
三维多层流动过孤立山脉产生的山脉重力波的数值试验 |
| 6. | The southern spread of low - layer inertia - gravity wave was benefited for coming into being of excessive strip rain belt
低层向南传播的重力惯性波有利于多条雨带的形成。 |
| 7. | It was benefited for southern spread of inertia - gravity wave in the symmetric instability region of the south of the high layer of rain belt
高层雨带南部的对称不稳定区，有利于重力惯性波的向南传播。 |
| 8. | The northern spread of high - layer inertia - gravity wave could result in the development and northern moving of low - layer vortex and precipitation
高层向北传播的重力惯性波可导致低层的涡旋和降水发展和北移。 |
| 9. | The north of the low - layer of rain belt was mainly convection instability . so the northern inertia - gravity wave was not easy to develop and to spread
雨区的北部低层以对流不稳定为主，因此向北的重力惯性波不易发展传播。 |
| 10. | These show that it is easier to inspire the severe convective weather by the action of nonlinear gravity waves in the condition of the existence of high - level jet
因此中尺度非线性重力波的相互作用是强对流天气突然爆发和一类飑线形成的可能动力机制之 |
