对流动性的担心和一波接一波的恐慌在二级市场司空见惯。
The secondary market, however, is prone to worries about liquidity and bouts of panic.
对流强迫重力内波的生成机制和向平流层的传播。
Generation Mechanisms of Convectively Forced Internal Gravity Waves and Their Propagation to the Stratosphere.
本文利用弹性波理论对流体——流体模型下直接场被井内流体割线积分抵消进行了证明。
By means of the theory elastic wave, this paper demonstrates direct field's being offset under fluid fluid matrix by secant integral in well.
大气波导的影响是对流层电磁波传播研究的热点和难点问题之一。
Atmospheric duct is one of the hot-topics and difficult problems in the propagation of electromagnetic waves in troposphere.
利用理论结果的计算表明，对流层的湍动对流完全有可能激发足够的波能去补充日冕中等离子体对流和辐射造成的能量损失。
Evaluation results show that the turbulence in convection zone is capable of generating enough wave energy to supply coronal energy lose due to convection and radiation.
指出与低纬深厚积云对流相联的凝结加热对亚洲夏季风环流所起的重要作用和大气定常行星波响应对加热场的垂直结构的敏感性。
It is shown that the aloft heating connected with latent heating, especially the deep condensation heating associated with cumulus convection in low latitudes, plays a crucial part for the Asian…
本文用特征线法研究了碱水二维渗流的对流模型，给出了碱水浓度非线性波传播公式。
We study the two-dimensional model of alkaline pulses by using the method of characteristics. The formulae of the nonlinear concentration waves are presented.
当然，这些增温并非是由臭氧损耗的辐射效应直接造成的，而是通过波-流相互作用以及平流层-对流层相互作用等动力学过程实现的。
The warming is not due to direct radiative effect of ozone depletion, instead, it is throughout dynamic processes, such as wave-mean flow and stratosphere-troposphere interactions.
它引发了一小场尘暴，例如，干扰了大气的向下对流，从而产生了这种波。
It'd trigger off a little dust devil, for example, that perturbs the atmosphere downstream in such a way that you get one of these waves.
根据对水面波的数学描述，给出了其对流场影响的精确解析解。
According to the mathematical description of surface waves, accurate analytical solutions of effects of surface waves upon flow fields are given in this paper.
对流层上层的斜压波、高空槽对天气的变化有重要的影响。
Baroclinic waves in upper? Troposphere, upper troughs and surface cyclones associated with wave packets are important systems for weather change and prediction.
这与对流层中激发的行星尺度波在冬季易于垂直向上传播的理论是定性上一致的。
Theory of vertical propagation of planetary stationary waves was used to explain the observations.
模式在对流层成功地模拟了行星波的年际变化形势，而对平流层的模拟并不理想。
In the troposphere, the interannual variation is well simulated by AGCM, but in the stratosphere the simulation is not successful.
这就证实了一些人认为的对流层机械波并不是一个对色球和日冕的有效加热机制的说法。
This confirms the idea that the mechanical waves generated from the convection zone are not very effective in heating the chromosphere and corona.
这就证实了一些人认为的对流层机械波并不是一个对色球和日冕的有效加热机制的说法。
This confirms the idea that the mechanical waves generated from the convection zone are not very effective in heating the chromosphere and corona.
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