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2.A NEW METHOD OF COMPUTING VERTICAL MOTION UNDER THE ASSUMPTION OF ISALLOBARIC WIND
双侧风假定下垂直运动计算方法收藏指正
3.The effects of non-linear advection on the wind structure and vertical motion in Ekman layer are studied.
本文研究了由于非线性平流作用所引起的对于Ekman层内风场及顶部垂直速度的影响。收藏指正
4.The effects of baroclinic on the wind structure and vertical motion in nonlinear Ekman layer are studied.
本文研究了斜压性对非线性Ekman层内的风场及顶部垂直速度的影响。收藏指正
5.Vertical motion of the carriage is provided by a pulldown gear case coupled by two pinions to racks on the mast.
滑架的垂直移动是由一个下拉齿轮箱提供的，该下拉齿轮箱则通过两个小齿轮连接到支架上的齿条上。收藏指正
6.The region of high temperature is estimated toreach at least as high as 9 km. There is strong vertical motion in the vicinity of the plateau.
3)夏季在高原上基本上是上升运动,可能达到9千米;收藏指正
7.In the present study,a solution of a vertically variable eddy viscosity boundary layer model under the Ekman momentum approximation is proposed. The effect of inertial term and vertical varying eddy viscosity on the wind structure,horizontal divergence,and vertical vorticity in the boundary layer and vertical motion at the top of boundary layer are discussed in detail.
本文利用边界层动力学中的 Ekman动量近似理论 ,给出了涡动粘性系数随高度缓变条件下的 Ekman动量近似边界层模式解 ,着重讨论了边界层的风场结构、水平散度、垂直涡度以及边界层顶部的垂直速度。收藏指正
8.The vertical motion in frontal zone would be induced by the orography dynamic lifting and the distribution of convergence which related to the interaction between the boundary layer friction, frontal structure and orography.
地形对锋区的垂直运动影响主要通过地形与边界层共同作用,改变锋区流场辐合辐散的分布及地形强迫抬升两条途径实现。收藏指正
9.The results of studying show that time dilation effect in horizontal motion of compound pendulum is a result of the change in mechanism of dynamics such as acceleration of gravity, such in vertical motion of compound pendulum is due to both the change in mechanism of dynamics and the change in mechanism of kinematics.
结果表明，复摆钟整体沿水平方向运动的钟慢效应是因为动力学机制发生了变化；而沿垂直方向运动的钟慢效应，既与动力学机制的变化有关，也与运动学机制的变化有关。收藏指正
10.There are three different physical factors affecting the nonlinear Ekman pumping (the vertical motion) at the top of baroclinic boundary layer: First, the barotropic geostrophic near the surface; Second, the thermal wind vorticity due to the atmospheric baroclinicity; Third, the nonlinear effect of joint of barotropic geostrophic vorticity and baroclinic thermal wind vorticity.
斜压边界层顶部的非线性Ekman抽吸(垂直运动)由三个不同的物理因子决定,第一、正压性的地面地转涡度,第二、斜压性作用产生的热成风涡度,第三、正压性的地面地转涡度与斜压性的热成风涡度的非线性相互作用。收藏指正
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