Effects of numerical model's horizontal resolution on the vertical transport of near-inertial energy

被引:3
|
作者
Lu, Xiaojie [1 ,2 ,6 ]
Dong, Changming [1 ,2 ,3 ]
Xu, Zhenhua [4 ,5 ]
Yang, Jingsong [2 ,6 ]
Zhang, Han [2 ,6 ]
Wang, Dongxia [7 ]
Chen, Dake [2 ,6 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Ocean Modeling & Observat Lab, Nanjing 210044, Peoples R China
[2] Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai 510045, Peoples R China
[3] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA
[4] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
[5] Chinese Acad Sci, Key Lab Ocean Circulat & Waves KLOCAW, Qingdao 266071, Peoples R China
[6] Minist Nat Resources, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Peoples R China
[7] CSSC Haizhuang Windpower Co Ltd, Chongqing 401147, Peoples R China
基金
美国国家科学基金会;
关键词
Energy transport; Near -inertial internal waves; Model resolution; Typhoon Kalmaegi (2014); HURRICANES KATRINA; TIDAL ENERGY; WAVE WAKE; TYPHOON; CIRCULATION; DISSIPATION; KUROSHIO; SURFACE; DRIVEN;
D O I
10.1016/j.dsr2.2022.105223
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Reproducing kinetic energy transport from the wind (mostly near inertial kinetic energy, NIKE) to the interior ocean is one of the most important issues in climate change numerical studies. Data recorded by two buoys in the South China Sea, which survived Typhoon Kalmaegi (2014), show that the NIKE can be transported into the deeper ocean in an anticyclonic rather than in a cyclonic eddy. Numerical experiments with three horizontal resolutions reveal that the increase in the model resolution enhances the enstrophy and advection, deepening NIKE transport and better reproducing the NIKE vertical distribution as observed. The present study finds that the horizontal resolution of a model can significantly impact the depth towards which the NIKE can be trans-ported, further implicating that the increase of the model resolution is an essential step to improve the accuracy of a climate model.
引用
收藏
页数:8
相关论文
共 50 条
  • [1] OBSERVATIONS ON VERTICAL POLARIZATION AND ENERGY FLUX OF NEAR-INERTIAL WAVES
    LEAMAN, KD
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 1976, 6 (06) : 894 - 908
  • [2] Enhanced Radiation of Near-Inertial Energy by Frontal Vertical Circulations
    Thomas, Leif N.
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 2019, 49 (09) : 2407 - 2421
  • [3] Horizontal variations of typhoon-forced near-inertial oscillations in the south China sea simulated by a numerical model
    Xu, Jiexin
    Huang, Yandan
    Chen, Zhiwu
    Liu, Junliang
    Liu, Tongya
    Li, Juan
    Cai, Shuqun
    Ning, Dezhi
    CONTINENTAL SHELF RESEARCH, 2019, 180 : 24 - 34
  • [4] Enhanced vertical propagation of storm-induced near-inertial energy in an eddying ocean channel model
    Zhai, XM
    Greatbatch, RJ
    Zhao, J
    GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (18) : 1 - 4
  • [5] Horizontal variability of near-inertial oscillations associated with the passage of a typhoon
    Hisaki, Y
    Naruke, T
    JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2003, 108 (C12)
  • [6] Organization of near-inertial energy by an eddy field
    Klein, P
    Smith, SL
    Lapeyre, G
    QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2004, 130 (598) : 1153 - 1166
  • [7] Observations of near-inertial energy in Lake Superior
    Austin, Jay
    LIMNOLOGY AND OCEANOGRAPHY, 2013, 58 (02) : 715 - 728
  • [8] An improved model of near-inertial wave dynamics
    Asselin, Olivier
    Young, William R.
    JOURNAL OF FLUID MECHANICS, 2019, 876 : 428 - 448
  • [9] Effects of Horizontal Resolution on Long-Range Equatorward Radiation of Near-Inertial Internal Waves in Ocean General Circulation Models
    Sun, Bingrong
    Jing, Zhao
    Yuan, Man
    Yang, Haiyuan
    Wu, Lixin
    JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2024, 16 (09)
  • [10] Seasonal Kinetic Energy Variability of Near-Inertial Motions
    Silverthorne, Katherine E.
    Toole, John M.
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 2009, 39 (04) : 1035 - 1049