• This in turn would give LIGO scientists an extra clue as to where to search their data for a gravity wave signal.

    这反过来给LIGO的科学家提供了一条在哪寻找引力波信号的新线索。

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  • The interaction of a gravity wave with a steady uniform current is dis - cussed in this paper.

    本文讨论了波浪与稳定均匀水流的相互作用问题。

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  • The equations can be used to study both interactions of fixed-phase and random-phase gravity wave packets.

    这组方程是研究固定相位和随机相位重力波相互作用问题的出发点。

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  • On average, gravity wave activities vary seasonally and weaken with increasing latitude, and exhibit interannual variations near the Equator.

    平均说来,随着纬度的增加重力波活动减弱,季节变化明显,近赤道地区重力波活动还呈现显著的年际变化特性。

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  • Saturation mechanism of gravity waves in mesosphere is discussed by simulating the nonlinear upward propagation of gravity wave in mesosphere.

    通过对向上传播的重力波波包在中层大气中的非线性传播过程进行数值模拟,讨论中层大气中重力波的饱和机制。

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  • The results show that a downward propagating gravity wave packet can be excited by two up-going gravity wave packets owing to the nonresonant interaction.

    研究表明:两个向上传播的重力波波包,通过非共振相互作用,也能激发出一个向下传播的重力波波包。

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  • The well-known phase speed formulas of surface inertial gravity wave and internal shear inertial gravity wave are the special cases of this frequency equation.

    表面惯性重力波和惯性重力内波的相速公式都是这个更普遍的频率方程的特殊情况。

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  • Xu Xiaofeng, Sun Zhaobo. 2003. Dynamic study on influence of gravity wave induced by unbalanced flow on Meiyu front heavy rain [J]. Acta Meteor Sinica, 61 (6) : 655-664.

    许小峰,孙照勃。2003。非地转平衡流激发的重力惯性波对梅雨锋暴雨影响的动力学研究[J]。气象学报,61 (6):655 - 664。

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  • The analysis method proposed can take into consideration of the effects of water surface gravity wave, water compressibility, and radiation damping at up-stream of reservoir.

    所建议的分析方法能够考虑表面重力波的影响、水体可压缩性、水库上游辐射阻尼等各种因素作用。

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  • It is explained by the capillary-gravity wave theory that the crests are sharpened and the troughs are plattened in the transverse harmonic of the non-propagating solitary waves.

    用毛细重力波理论解释了非传播孤立波横向谐振中波峰尖、波谷平的原因。

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  • This paper discusses the stability of internal inertial gravity wave in the heterogeneous stratified atmosphere when basic flow appears to be weak vertical shear by the WKB method.

    本文应用WKB方法研究了在弱非均匀层结大气中,当基本气流具有弱垂直切变时,重力惯性内波的稳定性问题。

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  • In the course of acoustic-gravity wave (AGW) propagation, a coupling relation between the ozone density oscillations (ODO) and temperature fluctuations (TF) in the lower thermosphere is presented.

    本文求出了声重波传播过程中,低热层臭氧含量振荡和温度场起伏间的耦合关系。

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  • The gravity wave dispersion can promote the propagation of the strong wind center along the LLJ, and the dispersion direction was influenced by the steering flow and the water vapor concentrated area.

    重力波的频散有利于急流中心大风区的传播,引导气流和水汽集中区对传播方向有显著影响;

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  • Gravity wave is the possible trigger mechanism of rainstorm.

    重力惯性波是暴雨产生的可能触发机制。

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  • The gravity, wave velocity and electrical resistivity changes before and after the earthquake may also be indicative of the deep rock of the existence of structural damage.

    地震前后的重力变化和波速变化以及电阻率变化可能也指示了深部岩体的结构损伤的存在。

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  • The gravity, wave velocity and electrical resistivity changes before and after the earthquake may also be indicative of the deep rock of the existence of structural damage.

    地震前后的重力变化和波速变化以及电阻率变化可能也指示了深部岩体的结构损伤的存在。

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