Journal of Tropical Oceanography ›› 2022, Vol. 41 ›› Issue (4): 136-145.doi: 10.11978/2021172CSTR: 32234.14.2021172

• Marine Hydrology • Previous Articles     Next Articles

Analysis of the dynamic characteristics of the east Guangdong shelf front in the northern South China Sea in summer

ZENG Yigang1,2(), JING Zhiyou1, HUANG Xiaolong1,2, ZHENG Ruixi1,2   

  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
  • Received:2021-12-04 Revised:2022-02-16 Online:2022-07-10 Published:2022-02-21
  • Contact: ZENG Yigang E-mail:2873417616@qq.com
  • Supported by:
    National Natural Science Foundation of China(92058201);National Natural Science Foundation of China(41776040);National Natural Science Foundation of China(41949907);National Natural Science Foundation of China(42149907);Original Innovation Project of Basic Frontier Scientific Research Program of Chinese Academy of Sciences(ZDBS-LY-DQC011);Guangzhou Science and Technology Project(201904010420)

Abstract:

This study investigates the characteristics of the east Guangdong shelf front and its dynamical regime using in-situ measurements, satellite data, and high resolution simulations by the regional ocean modeling system (ROMS). Observation results show active upwelling thermal fronts with horizontal scale of 50km on the northern shelf of the South China Sea in summer. The horizontal temperature gradient at the front is up to 0.06 ℃∙km-1 and is stronger than satellite observed results in the same period. The front can reach 20m depth, and has the characteristics of the order-one Richardson number. Further diagnostic analysis using ROMS model output also show that the horizontal buoyancy gradient is enhanced at the front, with order-one Richardson number, which is favorable for frontal instabilities. High-resolution simulation results indicate that driven by the southwest wind in summer, the Ekman transport across the continental shelf caused by down-front wind, will accumulate cold water of upwellings to the warm water, enhancing the horizontal buoyancy gradient and front sharpness, and change the frontal baroclinicity, which leads to negative Ertel potential vorticity (EPV). As such, the Ekman buoyancy flux caused by summer monsoon may significantly contribute to the formation and instability of the continental front in the northern South China Sea, and it has an important impact on the local dynamic environment.

Key words: northern South China Sea, shelf front, in-situ observation, front instability, ROMS

CLC Number: 

  • P731.2