Journal of Tropical Oceanography ›› 2021, Vol. 40 ›› Issue (6): 31-40.doi: 10.11978/2020152CSTR: 32234.14.2020152

• Marine Hydrology • Previous Articles     Next Articles

Submesoscale characteristics of a typical anticyclonic mesoscale eddy in Kuroshio Extension*

ZHANG Xu1,2(), JING Zhiyou1(), ZHENG Ruixi1,2, HUANG Xiaolong1,2, CAO Haijin3   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. College of Oceanography, Hohai University, Nanjing 210098, China
  • Received:2020-12-26 Revised:2021-03-01 Online:2021-11-10 Published:2021-03-03
  • Contact: JING Zhiyou E-mail:zhangxu184@mails.ucas.ac.cn;jingzhiyou@scsio.ac.cn
  • Supported by:
    Original Innovation Project of Basic Frontier Scientific Research Program of CAS(ZDBS-LY-DQC011);National Natural Science Foundation of China(92058201);National Natural Science Foundation of China(41776040);Innovation Academy of South China Sea Ecology and Environmental Engineering, CAS(ISEE2018PY05)

Abstract:

Using satellite measurements and high-resolution ROMS simulations, we analyze submesoscale characteristics of a typical anticyclonic mesoscale eddy in the Kuroshio Extension. Both satellite observations and high-resolution simulations show obvious submesoscale phenomena in the vortex region in the Kuroshio Extension. Our analysis results show that the strength of submesoscale kinetic energy is in close connection with kinetic energy of geostrophic velocity, which means that the frontogenesis may be an important way to enhance the submesoscale kinetic energy in the eddy periphery. Our analysis of the eddy’s vertical constructure shows submesoscale process can induce strong vertical velocity, which can be up to 100 m·day-1. The strong vertical velocity can reach a depth of hundreds of meters, indicating that submesoscale process can provide an efficient way for sea surface-internal material exchanging and air-sea interactions.

Key words: mesoscale eddy, submesoscale process, front, Kuroshio Extension

CLC Number: 

  • P731.2