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  1. NTU Theses and Dissertations Repository
  2. 理學院
  3. 海洋研究所
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/98674
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dc.contributor.advisor楊穎堅zh_TW
dc.contributor.advisorYiing-Jang Yangen
dc.contributor.author張仁宥zh_TW
dc.contributor.authorJen-Yu Changen
dc.date.accessioned2025-08-18T01:18:25Z-
dc.date.available2025-08-18-
dc.date.copyright2025-08-15-
dc.date.issued2025-
dc.date.submitted2025-08-06-
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Hu, Q., Huang, X., Xu, Q., Zhou, C., Guan, S., Xu, X., Zhao, W., Yang, Q., & Tian, J. (2023). Parametric Subharmonic Instability of Diurnal Internal Tides in the Abyssal South China Sea. Journal of Physical Oceanography, 53(1), 195-213. https://doi.org/10.1175/JPO-D-22-0020.1
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Liu, K., & Zhao, Z. (2020). Disintegration of the K1 internal tide in the South China Sea due to parametric subharmonic instability. Journal of Physical Oceanography, 50, 3605–3622. https://doi.org/10.1175/JPO-D-19-0320.1
Liu, Q., Xie, X. H., Shang, X. D., & Chen, G. Y. (2016). Coherent and incoherent internal tides in the southern South China Sea. Chinese Journal of Oceanology and Limnology, 34, 1374–1382. https://doi.org/10.1007/s00343-016-5171-5
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Olbers, D., Pollmann, F., & Eden, C. (2020). On PSI interactions in internal gravity wave fields and the decay of baroclinic tides. Journal of Physical Oceanography, 50(3), 751–771. https://doi.org/10.1175/JPO-D-19-0224.1
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The altimetric Mesoscale Eddy Trajectories Atlas (META3.2 DT) was produced by SSALTO/DUACS and distributed by AVISO+ (https://aviso.altimetry.fr) with support from CNES, in collaboration with IMEDEA (DOI: 10.24400/527896/a01-2022.005.220209 for the META3.2 DT allsat version)
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dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/98674-
dc.description.abstract本研究利用在太平島北部近東西向水道所觀測到的長期溫度與海流資料,研究週期約為全日潮週期兩倍的全日內潮次諧波運動。
觀測資料顯示四個主要特徵:第一、在深度-頻譜圖中,在潮汐頻率和近慣性頻率之間有一峰值,且非當地中尺度渦漩所造成;第二、頻帶濾波分析顯示全日內潮頻率一半的東西向海流和海溫在颱風雷伊經過後有顯著的變化,並且東西向海流垂直結構呈雙向傳播且高模態結構;第三、在颱風經過後,全日內潮次諧波深度積分動能的最大值與全日內潮變化相互對應,推測該次諧波增強可能和颱風增強當地全日內潮有關。第四、雙頻譜分析(bispectrum)證實在颱風經過後有非線性效應存在,推測與全日內潮參數次諧波不穩定(PSI)運動有關,使得全日內潮傳遞能量至其次諧波,增強颱風後全日內潮次諧波運動。
綜上所述,本研究觀測到頻率為全日內潮頻率一半的次諧波運動於颱風經過後增強,推測與颱風增強當地全日內潮以及全日內潮PSI運動有關。但本研究僅一觀測位置,後續須更多觀測與較大範圍的數值模式研究,才可了解颱風過後如何在該海域透過PSI增強全日內潮次諧波運動促進海水混合的整體動力機制。
zh_TW
dc.description.abstractThis study investigates the subharmonic motions of diurnal internal tides, with periods approximately twice that of the diurnal internal tides, using long-term temperature and current data observed in the east-west oriented channel north of Taiping Island.
The observed data revealed four main characteristics. First, the depth-frequency map showed a peak between tidal and near-inertial frequency, which was not caused by local mesoscale eddies. Second, bandpass analysis revealed significant changes in temperature and east-westward currents at half the diurnal internal tide frequency after the passage of Typhoon Rai. The vertical structure of east-westward currents displayed a bidirectional propagation and high-mode pattern. Third, the peaks of subharmonic motions in depth-integrated kinetic energy coincided with peaks of diurnal internal tides after the typhoon, suggesting the enhancement of subharmonic motions might be related to typhoon-induced local diurnal internal tides. Last, bispectrum analysis confirmed the presence of nonlinear interactions after the typhoon, suggesting the involvement of parametric subharmonic instability (PSI), which transfers energy from diurnal internal tides to its subharmonics, enhancing the subharmonic motions following the typhoon.
In conclusion, this study observed an enhancement of subharmonic motions at half of diurnal internal tide frequency after typhoon, might be related to the typhoon-induced intensification of local diurnal internal tides and PSI of the diurnal internal tides. However, due to the limitation of a single-station observation, further observations and modelling work is needed to understand the complete dynamical mechanism through which PSI enhances subharmonic motions to facilitate ocean mixing in the region after typhoon.
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dc.description.tableofcontents致謝 I
摘要 II
ABSTRACT III
目次 V
圖次 VII
表次 XI
符號表 XII
第一章、緒論 1
1.1研究背景 1
1.2 研究動機 3
第二章、資料介紹 5
2.1 錨碇資料介紹 6
2.2大氣資料介紹 9
2.3 新海研1號的水文觀測資料 9
2.4颱風最佳路徑資料介紹 10
2.5衛星資料介紹 10
2.6模式資料介紹 12
2.7經過錨碇串之颱風介紹 13
第三章、分析方法 15
3.1傅立葉頻譜分析(SPECTRUM ANALYSIS) 15
3.2旋轉能譜(ROTARY SPECTRUM) 16
3.3濾波分析(BAND-PASS ANALYSIS) 17
3.4小波分析 19
3.5斜壓流(BAROCLINIC CURRENTS) 21
3.6波向分解(DECOMPOSITION) 24
3.7雙頻譜分析(BISPECTRUM ANALYSIS) 26
第四章、分析結果與討論 28
4.1背景水文環境 28
4.2背景海流環境 32
4.3中尺度渦漩的影響 40
4.4颱風經過後變化 42
4.4.1時間序列分析 42
4.4.2 垂直傳遞方向分析 45
4.4.3 雙頻譜分析 49
4.5 PSI理論回顧與討論 50
4.5.1 PSI理論回顧 50
4.5.2 討論 53
第五章、結論 54
參考資料 56
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dc.language.isozh_TW-
dc.subject雙頻譜分析zh_TW
dc.subject參數次諧波不穩定(PSI)zh_TW
dc.subject非線性交互作用zh_TW
dc.subjectBispectrum analysisen
dc.subjectParametric Subharmonic Instability (PSI)en
dc.subjectNonlinear interactionen
dc.title南海中部全日內潮次諧波之研究zh_TW
dc.titleStudy on subharmonic waves of diurnal internal tides in the central South China Seaen
dc.typeThesis-
dc.date.schoolyear113-2-
dc.description.degree碩士-
dc.contributor.oralexamcommittee張明輝;方盈智;鄭宇昕zh_TW
dc.contributor.oralexamcommitteeMing-Huei Chang;Ying-Chih Fang;Yu-Hsin Chengen
dc.subject.keyword參數次諧波不穩定(PSI),非線性交互作用,雙頻譜分析,zh_TW
dc.subject.keywordParametric Subharmonic Instability (PSI),Nonlinear interaction,Bispectrum analysis,en
dc.relation.page62-
dc.identifier.doi10.6342/NTU202504191-
dc.rights.note同意授權(全球公開)-
dc.date.accepted2025-08-12-
dc.contributor.author-college理學院-
dc.contributor.author-dept海洋研究所-
dc.date.embargo-lift2025-08-18-
顯示於系所單位:海洋研究所

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