Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (5): 1-16.doi: 10.11978/2022260CSTR: 32234.14.2022260

Special Issue: 全球变化专题

• Marine Hydrology •     Next Articles

The evolution and energy characteristics of the Sri Lanka Dome*

MA Yu1,2(), WANG Weiqiang3,4(), YOU Qinglong1, XIN Hongyu5,6   

  1. 1. Department of Atmospheric and Oceanic Sciences, Fudan University, Shanghai 200438, China
    2. East China Air Traffic Management Bureau of Civil Aviation Administration of China, Shanghai 200335, China
    3. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    4. Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 511458, China
    5. Institute of Deep-sea Science and Engineering, Chinese Academic Science, Sanya 572000, China
    6. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2022-12-23 Revised:2023-04-04 Online:2023-09-10 Published:2023-04-17
  • Supported by:
    National Key R&D Program of China(2022YFE0203500); National Natural Science Foundation of China(91958202); Development Fund of South China Sea Institute of Oceanology of the Chinese Academy of Sciences(SCSIO202201); Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences(ISEE2021ZD01)

Abstract:

This study systematically investigates the evolution and energy characteristics of the climatic Sri Lanka Dome (SLD) using hybrid coordinate ocean model (HYCOM) and National Centers for Environmental Prediction (NCEP) reanalysis datasets. The results show that the SLD undergoes two peaks of intensity and eddy kinetic energy (EKE) during its lifecycle. During the first development stage (May 23 to June 10), SLD shifts from the southeast to the east of Sri Lanka, and its area gets wider while its intensity gets stronger. The strengthening of the SLD is attributed to a combination of wind stress work, eddy-mean flow interaction, and advection of the southwest monsoon current (SMC). During the mature stage (June 11 to 22), when the SLD is located to the east of Sri Lanka, the EKE and eddy available potential energy (EPE) in the SLD region reaches its first peak due to enhanced wind stress work and eddy-mean flow interaction. During the weakening stage (June 23 to July 20), the SLD moves northwestward and loses EKE and EPE due to the dissipation of the advection term, reduction of wind stress work and baroclinic instability. During the stable stage (July 21 to August 14), the SLD shifts to the northeast of Sri Lanka, with weaker wind stress work, pressure work, and eddy-mean flow interaction, which keeps the strength of the SLD at a weak level. During the second development stage (August 15 to 25), the SLD moves northward with increased intensity, mainly due to enhanced wind stress and pressure work. During the decay stage (August 26 to September 5), the process of ocean internal instability transforms EKE and EPE into mean flow energy, weakening the SLD. In summary, wind stress work, eddy-mean flow interaction, pressure work, and the advection of SMC are all essential factors in the evolution of SLD.

Key words: Sri Lanka Dome, eddy-mean flow interaction, energy analysis, mesoscale eddy, southwest monsoon current