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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >A numerical study on nonresonant interactions of gravity waves in a compressible atmosphere
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A numerical study on nonresonant interactions of gravity waves in a compressible atmosphere

机译:数值研究nonresonant交互的可压缩大气重力波

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Applying a second-order numerical scheme, nonresonant interactions of gravity waves in a compressible atmosphere are investigated. The numerical results show that the nonresonant interaction of the gravity waves does occur, and an apparent energy exchange among the interacting waves can be observed, which indicates that the gravity waves with different spatial and temporal scales can extensively interact. In the nonresonant interaction, the wave energy generally tends to transfer from the primary wave with the highest frequency to the secondary and excited waves, which is different from that in the resonant interaction. Under the same initial energy of the secondary wave, the final energy of the excited wave is almost proportional to the initial energy of the primary wave. When the initial energies of the primary waves are identical, the final energy of the excited wave increases slowly with the increasing initial energy of the secondary wave. Similar to that in the resonant interaction, in the nonresonant interaction, wave vector and frequency of the excited wave show temporal variability. The wave vectors of the interacting triad do not satisfy the matching conditions which should be obeyed in the weak interaction theory. We also investigate the effects of the background wind field and viscous dissipation on the nonresonant interaction. The positive and negative background winds show tendencies to strengthen and weaken the wave energy transfer, respectively. This also differs from the weak interaction theory, in which only a Doppler shift can be caused. The primary effect of the viscosity is to dissipate the energy of the interacting waves. The viscosity can hardly prevent the nonresonant excitation, suggesting that the restriction of amplitude threshold on the interaction in the presence of viscosity predicted by the weak interaction approximation seems to be rather loose. As in the resonant interaction, the principal energy exchange is finished before the waves depart from each other, which indicates that the interacting characteristic time does exist in the nonresonant interaction. The characteristic time and evolutions of wavelength and intrinsic frequency for the excited wave are insensitive to the small initial wave amplitudes and Gaussian packet widths of the interacting waves, horizontal background wind field, and viscosity. However, the characteristic time is relevant to the wavelengths of the interacting waves.
机译:应用二阶数值方案,nonresonant重力波的相互作用可压缩的气氛了。数值结果表明,该nonresonant重力波的相互作用发生一个明显的相互作用之间的能量交换声波可以观察到,这表明重力波具有不同的空间和时间尺度可以广泛交流。nonresonant交互,波的能量一般倾向于转移从主波二、最高的频率兴奋波,这是不同的共振相互作用。次要的能量波,最后的能量兴奋波几乎是成正比的初始能量的主要波。主要的初始能量波相同,最后兴奋波的能量与增加的初始增加缓慢次波的能量。共振相互作用,nonresonant相互作用,波矢和频率兴奋波显示颞可变性。向量的三合会不满足交互应遵守的匹配条件弱相互作用理论。背景风场的影响nonresonant粘性耗散交互。风倾向加强和削弱波的能量传递。不同于弱相互作用理论这只能导致一个多普勒频移。粘度的主要影响是消散相互作用的能量波。粘度几乎不能防止nonresonant激励,这表明的限制振幅阈值的交互的粘度预测的虚弱相互作用近似似乎相当松了。主要能量交换完成之前波离开彼此,这表明交互特征时间存在于nonresonant交互。时间和波长的演进特征兴奋波和固有频率对小的初始波振幅和高斯包宽度的互动波,水平背景风场,和粘度。与波长相关的相互作用波。

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