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Generation and evolution on symmetric ocean inner waves in unstable background flow
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Yanling Zhao1, Xu Lu2, Hong Huang3, *, Saisai Liu1, Ming Zhang3
Haiyang Xuebao | 2020, 42(11) : 12 - 22
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Haiyang Xuebao | 2020, 42(11): 12-22
Article
Generation and evolution on symmetric ocean inner waves in unstable background flow
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Yanling Zhao1, Xu Lu2, Hong Huang3, *, Saisai Liu1, Ming Zhang3
Affiliations
  • 1 The PLA 31010 Units, Beijing 100081, China
  • 2 The PLA 32021 Units, Beijing 100094, China
  • 3 Laboratory of Atmospheric Circulation and Short-range Climate Forecast, Meteorological and Oceanographic College, National University of Defense Technology, Nanjing 211101, China
Published: 2020-11-25 doi: 10.3969/j.issn.0253-4193.2020.11.002
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Using the two-dimensional non-static numerical model, which neglect the submarine topography but consider the pycnocline and background shear flow, the numerical experiment was made on the generation and evolution of linear and nonlinear symmetric ocean internal waves in the unstable downward shear background flow. After analyzing and comparing the results, the main conclusions are as follows: the linear internal wave strength is exponentially growing with integral time, and there’s symmetric instability of the wave, while nonlinear internal wave strength is growing quasi-linearly in the development stage, and finally enters the stabilization stage. The linear growing is much faster than the nonlinear growing and the latter has a stabilizing effect. For linear and nonlinear symmetric internal waves, there are maximum value of potential density perturbation, which is captured by the pycnocline. This is consistent with actual observations. The stream function and potential density perturbation are well coordinated, which is reflected in the positive and negative centers of the potential density perturbation corresponding to the rising and sinking movements of the stream function, respectively. This shows that there is a slantwise convection occurred from the bottom of the sea and the pycnocline is the top cover. For linear internal waves, with the increase of integral time, its waveform is basically the same and the positive and negative amplitude is also about the same. There are two slantwise circulations that grow in opposite signs and between them is a strong slantwise upwelling. The waveform of nonlinear internal wave changes with the integration time and the number of slantwise circulations is also increasing, resulting in the stronger negative circulations and a sharp increase in the horizontal gradient of stream function and potential density perturbation. The sharp increase can be regarded as an interruption.

numerical experiment  /  ocean internal wave  /  unstable shear background flow  /  symmetric instability
Yanling Zhao, Xu Lu, Hong Huang, Saisai Liu, Ming Zhang. Generation and evolution on symmetric ocean inner waves in unstable background flow[J]. Haiyang Xuebao, 2020 , 42 (11) : 12 -22 . DOI: 10.3969/j.issn.0253-4193.2020.11.002
Year 2020 volume 42 Issue 11
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Article Info
doi: 10.3969/j.issn.0253-4193.2020.11.002
  • Receive Date:2019-12-23
  • Online Date:2026-03-27
  • Published:2020-11-25
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History
  • Received:2019-12-23
  • Revised:2020-02-16
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Affiliations
    1 The PLA 31010 Units, Beijing 100081, China
    2 The PLA 32021 Units, Beijing 100094, China
    3 Laboratory of Atmospheric Circulation and Short-range Climate Forecast, Meteorological and Oceanographic College, National University of Defense Technology, Nanjing 211101, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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