Generation of mode-2 internal waves in a two-dimensional stratification by a mode-1 internal wave

被引:6
|
作者
Liang, Jianjun [1 ,2 ]
Du, Tao [3 ]
Li, Xiaoming [1 ,4 ]
He, Mingxia [2 ]
机构
[1] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, Key Lab Digital Earth Sci, Beijing, Peoples R China
[2] Ocean Univ China, Ocean Remote Sensing Inst, Qingdao, Peoples R China
[3] Ocean Univ China, Coll Ocean & Atmospher Sci, Qingdao, Peoples R China
[4] Key Lab Earth Observat, Sanya, Hainan, Peoples R China
基金
中国国家自然科学基金;
关键词
Mode-2 internal wave; Two-dimensional stratification; Generation; Favorable environmental conditions; SLOPE-SHELF TOPOGRAPHY; SOUTH CHINA SEA; SOLITARY WAVES; LOCAL GENERATION; CENTRAL BAY; THERMOCLINE; PYCNOCLINE; EVOLUTION; SOLITONS; PACKETS;
D O I
10.1016/j.wavemoti.2018.09.014
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
The generation of mode-2 nonlinear internal waves (IWs) by the evolution of a mode-1 IW in a two-dimensional stratification is investigated. A generation model accounting for intermodal interaction is derived based on a multi-modal approach in a weakly nonlinear and non-hydrostatic configuration. The generation model is numerically solved to simulate the evolution of mode-1 and mode-2 IWs in an inhomogeneous pycnocline. The numerical experiments confirm that mode-2 IWs are generated due to linear and nonlinear intermodal interaction. The mode-2 IW continues growing and gradually separates with the mode-1 IW during the generation process. The numerical results suggest that the pycnocline strength or thickness prominently affects the generation of mode-2 IWs, followed by pycnocline depth. A weakening or thinning pycnocline favors the generation of mode-2 IWs by evidently enhancing linear and nonlinear intermodal interaction, whereas a shoaling pycnocline favors a rapid growth rate mainly by enhancing linear intermodal interaction. The wave amplitude of an initial mode-1 IW strongly affects the generation of mode-2 IWs and increasing it can noticeably enlarge mode-2 IWs. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:227 / 240
页数:14
相关论文
共 50 条
  • [1] The interaction of a mode-1 internal solitary wave with a step and the generation of mode-2 waves
    Liu, Zihua
    Grimshaw, Roger
    Johnson, Edward
    GEOPHYSICAL AND ASTROPHYSICAL FLUID DYNAMICS, 2019, 113 (04): : 327 - 347
  • [2] Resonant coupling of mode-1 and mode-2 internal waves by topography
    Liu, Zihua
    Grimshaw, Roger
    Johnson, Edward
    JOURNAL OF FLUID MECHANICS, 2021, 908
  • [3] Shear instability in mode-2 internal Kelvin waves
    Stastna, Marek
    Deepwell, David
    Grace, Andrew
    ENVIRONMENTAL FLUID MECHANICS, 2023, 23 (02) : 407 - 428
  • [4] Shear instability in mode-2 internal Kelvin waves
    Marek Stastna
    David Deepwell
    Andrew Grace
    Environmental Fluid Mechanics, 2023, 23 : 407 - 428
  • [5] Numerical Investigation of Bidirectional Mode-1 and Mode-2 Internal Solitary Wave Generation from North and South of Batti Malv Island, Nicobar Islands, India
    Raju, N. Jithendra
    Dash, Mihir K.
    Bhaskaran, Prasad Kumar
    Pandey, P. C.
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 2021, 51 (01) : 47 - 62
  • [6] FRACTURE BY BLENDED MODE-1 AND MODE-2 ON SHEAR LIPS
    BEACHEM, CD
    BROOKS, EJ
    REPORT OF NRL PROGRESS, 1975, (NOV): : 13 - 14
  • [7] Generation of mode 2 internal waves by the interaction of mode 1 waves with topography
    Liu, Zihua
    Grimshaw, Roger
    Johnson, Edward
    JOURNAL OF FLUID MECHANICS, 2019, 880 : 799 - 830
  • [8] Shoaling mode-2 internal solitary-like waves
    Carr, Magda
    Stastna, Marek
    Davies, Peter A.
    van de Wal, Koen J.
    JOURNAL OF FLUID MECHANICS, 2019, 879 : 604 - 632
  • [9] Wave generation through the interaction of a mode-2 internal solitary wave and a broad, isolated ridge
    Deepwell, David
    Stastna, Marek
    Carr, Magda
    Davies, Peter A.
    PHYSICAL REVIEW FLUIDS, 2019, 4 (09):
  • [10] On the predictability of mode-1 internal tides
    Dushaw, Brian D.
    Worcester, Peter F.
    Dzieciuch, Matthew A.
    DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2011, 58 (06) : 677 - 698