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A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves

Received: 9 December 2018     Published: 11 December 2018
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Abstract

Laboratory experiment is an important method in the study of ocean internal waves, and the schlieren technique is an effective way to observe the internal waves in the laboratory. The digital synthetic schlieren technique is mostly applied to two-dimensional density-stratified flows. The technique is improved by setting up the Charge Coupled Device (CCD) vertically to shoot the reference images in this research. Then the three-dimensional density-stratified flows can be detected in this way. The authors attempt a set of lab experiments to verify the rationality of this technique. There is a horizontally moving spherule with constant velocity at the interface of the two-layer stratified water in the experiment. The moving spherule generates internal waves between the two-layer fluids. The authors successfully capture the three-dimensional structure of the internal waves generated by the horizontally moving spherule. It is obvious that the internal waves have characteristics of the Kelvin Internal Wake and the quantitative parameters agree well with the previous studies. The experimental results reveal that the improved digital schlieren technique is rational and feasible in the lab internal waves observations. The detailed three-dimensional structure of the internal waves, the internal wave energy distribution and propagation in the whole field and the nonlinear interactions between the internal waves can be further studied through this method in the future.

Published in Earth Sciences (Volume 7, Issue 6)
DOI 10.11648/j.earth.20180706.15
Page(s) 283-288
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2018. Published by Science Publishing Group

Keywords

Internal Waves, Synthetic Schlieren, Kelvin Internal Wake

References
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[4] P. J. Diamessis, S. Wunsch, I. Delwiche, and M. P. Richter, “Nonlinear generation of harmonics through the interaction of an internal wave beam with a model oceanic pycnocline,” Dynamics of Atmospheres and Oceans, 2014, vol. 66, pp. 110–137.
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[6] H. Sun, Q. Wang, “Microstructure observations in the upper layer of the South China Sea,” Journal of Oceanography, 2016, vol. 72, pp. 1-10.
[7] J. Yang, J. Wang, R. Lin, “The first quantitative remote sensing of ocean internal waves by Chinese GF-3 SAR satellite,” Acta Oceanologica Sinica, 2017, vol. 36, pp. 118-118.
[8] J. K. Wang, M. Zhang, Z. H. Cai, et al, “SAR imaging simulation of ship-generated internal wave wake in stratified ocean,” Journal of Electromagnetic Waves & Applications, 2017, vol. 31, pp. 1-14.
[9] Ø. A. Arntsen, “Disturbances, lift and drag forces due to the translation of a horizontal circular cylinder in stratified water,” Experiments in fluids, 1996, vol. 21, pp. 387-400.
[10] Z. Xu, Q. Li, V. A. Gorodtsov, “Wave drag of rapidly and horizontally moving Rankine ovoid in uniformly stratified fluid,” Progress in Natural Science, 2008, vol. 18, pp. 723-727.
[11] J. Wang, X. Chen, W. Wang, et al, “Laboratory experiments on the resonance of internal waves on a finite height subcritical topography,” Ocean Dynamics, 2015, vol. 65, pp. 1269-1274.
[12] Y. Dossmann, B. Bourget, C. Brouzet, et al, “Mixing by internal waves quantified using combined PIV/PLIF technique,” Experiments in Fluids, 2016, vol. 57, pp. 132.
[13] G. S. Settles, M. Hargather, “A review of recent developments in schlieren and shadowgraph techniques,” Measurement Science & Technology, 2017, vol. 28.
[14] J. M. Toole, R. W. Schmitt, “Polzin, K. L. Estimates of diapycnal mixing in the abyssal ocean,” Science, 1994, vol. 264, pp. 1120-1123.
[15] S. B. Dalziel, G. O. Hughes, B. R. Sutherland, “Whole-field density measurements by ‘synthetic schlieren’,” Experiments in Fluids, 2000, vol. 28, pp. 322-335.
[16] B. R. Sutherland, S. B. Dalziel, G. O. Hughes, P. F. Linden, “Visualization and measurement of internal waves by ‘synthetic schlieren’. Part 1. Vertically oscillating cylinder,” Journal of Fluid Mechanics, 1999, vol. 390, pp. 93-126.
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Cite This Article
  • APA Style

    Qingjun Meng, Yanzhen Gu, Peiliang Li, Xinzhu Wu. (2018). A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves. Earth Sciences, 7(6), 283-288. https://doi.org/10.11648/j.earth.20180706.15

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    ACS Style

    Qingjun Meng; Yanzhen Gu; Peiliang Li; Xinzhu Wu. A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves. Earth Sci. 2018, 7(6), 283-288. doi: 10.11648/j.earth.20180706.15

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    AMA Style

    Qingjun Meng, Yanzhen Gu, Peiliang Li, Xinzhu Wu. A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves. Earth Sci. 2018;7(6):283-288. doi: 10.11648/j.earth.20180706.15

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  • @article{10.11648/j.earth.20180706.15,
      author = {Qingjun Meng and Yanzhen Gu and Peiliang Li and Xinzhu Wu},
      title = {A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves},
      journal = {Earth Sciences},
      volume = {7},
      number = {6},
      pages = {283-288},
      doi = {10.11648/j.earth.20180706.15},
      url = {https://doi.org/10.11648/j.earth.20180706.15},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20180706.15},
      abstract = {Laboratory experiment is an important method in the study of ocean internal waves, and the schlieren technique is an effective way to observe the internal waves in the laboratory. The digital synthetic schlieren technique is mostly applied to two-dimensional density-stratified flows. The technique is improved by setting up the Charge Coupled Device (CCD) vertically to shoot the reference images in this research. Then the three-dimensional density-stratified flows can be detected in this way. The authors attempt a set of lab experiments to verify the rationality of this technique. There is a horizontally moving spherule with constant velocity at the interface of the two-layer stratified water in the experiment. The moving spherule generates internal waves between the two-layer fluids. The authors successfully capture the three-dimensional structure of the internal waves generated by the horizontally moving spherule. It is obvious that the internal waves have characteristics of the Kelvin Internal Wake and the quantitative parameters agree well with the previous studies. The experimental results reveal that the improved digital schlieren technique is rational and feasible in the lab internal waves observations. The detailed three-dimensional structure of the internal waves, the internal wave energy distribution and propagation in the whole field and the nonlinear interactions between the internal waves can be further studied through this method in the future.},
     year = {2018}
    }
    

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  • TY  - JOUR
    T1  - A New Application of the Digital Synthetic Schlieren in Lab Experiments of the Internal Waves
    AU  - Qingjun Meng
    AU  - Yanzhen Gu
    AU  - Peiliang Li
    AU  - Xinzhu Wu
    Y1  - 2018/12/11
    PY  - 2018
    N1  - https://doi.org/10.11648/j.earth.20180706.15
    DO  - 10.11648/j.earth.20180706.15
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 283
    EP  - 288
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20180706.15
    AB  - Laboratory experiment is an important method in the study of ocean internal waves, and the schlieren technique is an effective way to observe the internal waves in the laboratory. The digital synthetic schlieren technique is mostly applied to two-dimensional density-stratified flows. The technique is improved by setting up the Charge Coupled Device (CCD) vertically to shoot the reference images in this research. Then the three-dimensional density-stratified flows can be detected in this way. The authors attempt a set of lab experiments to verify the rationality of this technique. There is a horizontally moving spherule with constant velocity at the interface of the two-layer stratified water in the experiment. The moving spherule generates internal waves between the two-layer fluids. The authors successfully capture the three-dimensional structure of the internal waves generated by the horizontally moving spherule. It is obvious that the internal waves have characteristics of the Kelvin Internal Wake and the quantitative parameters agree well with the previous studies. The experimental results reveal that the improved digital schlieren technique is rational and feasible in the lab internal waves observations. The detailed three-dimensional structure of the internal waves, the internal wave energy distribution and propagation in the whole field and the nonlinear interactions between the internal waves can be further studied through this method in the future.
    VL  - 7
    IS  - 6
    ER  - 

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Author Information
  • College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao, China

  • College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao, China

  • Ocean College, ZheJiang University, Zhoushan, China

  • School of Hydraulic Engineering, Dalian University of Technology, Dalian, China

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