Experimental Investigation on the Vertical Structure Characteristics of Internal Solitary Waves

Experimental Investigation on the Vertical Structure Characteristics of Internal Solitary Waves
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内孤立波垂直结构特性的实验研究

DOI:
10.3390/jmse10081045
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发表时间:
2022-07
影响因子:
2.9
通讯作者:
Jieshuo Xie
Jieshuo Xie
中科院分区:
地球科学3区
文献类型:
--
作者:
Pai Peng;Hui Du;Gang Wei;Shaodong Wang;Pu Xuan;Shuqun Cai;Jieshuo Xie

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系统地研究了内孤立波在大型重力分层流体水槽中的垂直结构特征。建立了四种不同的分层,并用电导探针阵列测量了ISW的基本元素。给出了不同层数下两种ISW的振幅、特征频率和波形的垂直分布,并与理论模型进行了比较。研究表明,不同层位的地震波振幅垂直结构与理论模型基本一致,而振幅较大的地震波则存在一定的偏差。两层模型和连续分层模型都不能有效地描述不同深度特征频率随幅度的变化。对于单个小幅度地震波,其特征频率随深度的增加先增大后减小。特征频率在浮力频率最大的深度处最大。对于振幅较大的ISW,在浮力频率最大的深度附近有可能出现特征频率的局部极小值。在不同的地层中,KdV理论的Sech2函数可以很好地描述不同深度的ISW波形。
An experimental investigation of the vertical structure characteristics of internal solitary waves (ISWs) was systematically carried out in a large gravitationally stratified fluid flume. Four different stratifications were established, and basic elements of ISWs were measured by a conductivity probe array. The vertical distributions of the amplitude, characteristic frequency and waveform of two types of ISWs under different stratifications were obtained, and the experimental results were compared with the theoretical model. The study shows that most vertical structures of the amplitude under different stratifications agree with those of the theoretical model, while there are some deviations for ISWs with large amplitudes. Neither the two-layer model nor the continuously stratified model can effectively describe the variation in the characteristic frequency at different depths with amplitude. For a single small-amplitude ISW, the characteristic frequency first increases and then decreases with increasing depth. The characteristic frequency is largest at the depth of the maximum buoyancy frequency. For an ISW with a relatively large amplitude, there is likely to be a local minimum of the characteristic frequency near the depth where the maximum buoyancy frequency lies. In different stratifications, the sech2 function of KdV theory can describe the waveforms of ISWs at different depths well.
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