| 1. | Analytical solution of the basic equations set of atmospheric motion
大气运动基本方程组的解析解 |
| 2. | Stability for the basic system of equations of atmospheric motion
大气运动基本方程组的稳定性分析 |
| 3. | N eddying motion of the atmosphere that interrupts the flow of wind
指的是a湍流打断风的运动的极不规则的大气运动。 |
| 4. | Flight dynamics - concepts , quantities and symbols - part 9 : models of atmospheric motions along the trajectory of the aircraft
飞行动力学.概念量及符号.第9部分:飞行器沿飞行轨迹的大气运动模型 |
| 5. | Streamline charts are usually drawn for upper air to display the spatial distribution of flow directions at a particular instance of time
流线流线图一般惯用于高空，展示某一时刻大气运动流向的空间分布。 |
| 6. | Tides are caused by gravitational attraction of the sun and moon ; the weather by the motion of atmosphere under the influence of heat from the sun
潮汐是由太阳和月亮的重力吸引所致；而天气则是因太阳的热量影像大气运动而形成的。 |
| 7. | In this paper , a lienard type equation is deduced from the basic equation of atmospheric motion in stratified atmosphere , and then we consider the existence of the periodic solutions for lienard and duffing type equations
本文由层结大气运动基本方程导出li nard型方程，进而考虑li nard及duffing型方程周期解的存在性问题。 |
| 8. | Solar radiation is the most important energy source on earth , its time and space distribution on earth restricts the climate system ' s movment , also is the most important gene in the climate system ' s form and evolvement
太阳辐射是地球大气运动的最重要能源，它在地球上的时间和空间分布，制约着地球上气候系统的运动，也是地球气候形成和演变过程中重要的因子。 |
| 9. | The diffusion model and numerical simulation model for chaff clouds are modeled on the assumption that the speed of air where chaff locates is a winner random process and the mass of chaff is zero so it can trace the atmosphere speed very well
摘要假定箔条所在位置处大气运动速度是一个维纳随机过程，同时在忽略箔条的质量时箔条的运动完全反应当地大气的运动，在此基础上建立箔条云团的扩散模型及数值仿真模型。 |
| 10. | The results show that unbalance force of atmospheric motion and the coupling reaction among convective cloud cluster and moisture frontal zone and low level jet lead to the continuation of strong convergence in low layer and the maintenance of torrential rain
分析结果发现，大气运动非平衡强迫、凝结降水的非均匀分布与强烈垂直风切变的耦合作用、 “湿度锋”与低空急流的耦合相互作用通过促进低空辐合流的维持，导致了对流云团和暴雨天气的持续。 |
