Journal of Tropical Oceanography ›› 2025, Vol. 44 ›› Issue (5): 39-49.doi: 10.11978/2024226CSTR: 32234.14.2024226

• Marine Hydrology • Previous Articles     Next Articles

Three-dimensional eddy structure reconstruction in the Northwest Pacific using variational method and satellite sea surface data

LI Lin1,2(), WANG Xidong1,2(), HE Zikang1,2, CHEN Zhiqiang3, CAO Yuan1,2, LIU Kefeng4, CHEN Jian5   

  1. 1. Key Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing 210024, China
    2. College of Oceanography, Hohai University, Nanjing 210024, China
    3. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
    4. College of Advanced Interdisciplinary Studies, National University of Defense Technology, Changsha 410073, China
    5. 5 Room, Beijing Institute of Applied Meteorology, Beijing 100029, China
  • Received:2024-12-02 Revised:2025-02-07 Online:2025-09-10 Published:2025-10-14
  • Contact: WANG Xidong
  • Supported by:
    National Key Research and Development Program of China(2022YFE0106400); National Natural Science Foundation of China(62073332)

Abstract:

This study reconstructs the three-dimensional dynamic temperature field in the Northwest Pacific Ocean using high-resolution satellite sea surface data and historical ocean temperature and salinity profile data, based on the variational method. Compared to the array for real-time geostrophic oceanography (Argo) temperature profiles, the reconstructed temperature field reasonably reproduces the vertical distribution of seawater temperature, particularly in the thermocline region, where the results closely match the actual observed temperature profiles. Two typical mesoscale eddy cases were selected for analysis of their entire evolution process — from generation to decay — using the reconstructed temperature field, displaying the dynamic changes in the vertical and horizontal distribution of temperature anomalies induced by the eddies. In particular, during the mature stage of the eddies, the intensity and vertical extent of the temperature anomalies reach their maximum, reflecting the significant impact of the eddies on the oceanic thermocline. By analyzing the distribution of temperature anomalies at different stages, the study reveals the evolution of the spatial structure of cold and warm cores and the anomalous regions. The results show that the method can effectively utilize satellite sea surface observations to reconstruct the underwater temperature structure and dynamic evolution of mesoscale eddies, providing valuable data support for understanding their role in oceanic material and heat transport.

Key words: variational method, satellite sea surface information, mesoscale eddy, three-dimensional temperature structure

CLC Number: 

  • P731.27