Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (3): 10-18.doi: 10.11978/2019056CSTR: 32234.14.2019056

• Marine Hydrology • Previous Articles     Next Articles

Anisotropy of submesoscale eddy in Kuroshio Extension based on high resolution ROMS output analysis

Xiaowen ZHOU1, Haijin CAO1(), Zhiyou JING2, Guanghong LIAO1   

  1. 1. College of Oceanography, Hohai University, Nanjing 210098, China
    2. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China;
  • Received:2019-06-17 Revised:2019-12-13 Online:2020-05-10 Published:2020-05-19
  • Contact: Haijin CAO E-mail:h.cao@hhu.edu.cn
  • Supported by:
    The National Key Research and Development Program of China(2017YFA0604104);Opening Foundation of State Key Laboratory of Tropical Oceanography(South China Sea Institute of Oceanology, Chinese Academy of Sciences)(LTO1907);Chinese Postdoctoral Foundation(2018M642148);Jiangsu Planned Projects for Postdoctoral Research Funds(2018K149C);National Natural Science Foundation of China(41776040);Opening of OCFL Functional Laboratory of Qingdao Pilot National Laboratory of Marine Science and Technology(201804)

Abstract:

Submesoscale eddies have smaller Richardson number and larger Rossby number, with horizontal scales between 0.1 and 10 km and time scale of ~0(1 day). They act to extract energy from the mesoscale circulation, drive forward energy cascade to the smaller scale turbulence and meanwhile contribute to the vertical flux of what in the upper ocean. In this study, anisotropy of submesoscale eddies in the Kuroshio Extension in a high-resolution simulation (?x≈500m) by the regional ocean modeling system (ROMS) is evaluated using the nummular variance ellipse method. A correlation between eddy anisotropy and submesoscale features is also analyzed. The results show that the submesoscale eddies, as well as the anisotropy, near the flow stream get intensified compared to those in the flanks. The isotropic ratio is well correlated with the strength of submesoscale processes, suggesting that the submesoscale processes tend to be isotropic. The nummular variance ellipse, known as the feedback of eddies to mean flow, may implies forward cascade of kinetic energy.

Key words: submesoscale eddy, Kuroshio Extension, eddy anisotropy, energy cascade, upper ocean