Journal of Tropical Oceanography ›› 2018, Vol. 37 ›› Issue (3): 9-18.doi: 10.11978/2017077CSTR: 32234.14.2017077

• Orginal Article • Previous Articles     Next Articles

Cross-basin particle transport by a warm eddy southwest of Taiwan Island

Xiayan LIN1,2(), Changming DONG3(), Dake CHEN2   

  1. 1. Ocean College, Zhejiang University, Zhoushan 316021, China
    2. State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration Hangzhou 310012, China
    3. School of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China;
  • Received:2017-07-09 Revised:2017-09-25 Online:2018-06-10 Published:2018-05-03
  • Supported by:
    National Program on Key Basic Research Project (“973” Program) (2013CB430302);National Programme on Global Change and Air-Sea;Interaction ( GASI-IPOVAI-04 );National Natural Science Foundation of China (41621064, 41476022 );National Key Research Program of China

Abstract:

The site southwest of Taiwan Island is one of the places where warm core eddies originate. Extensive studies on warm eddies have been conducted; however, a majority of these studies focused on eddy characteristics, such as radius, generation area and lifetime. Some discussed generation mechanisms while the investigation of transport by warm eddies remains scarce. We observed a warm eddy during autumn 2003 to spring 2004 using both AVISO (Archiving Validation and Interpretation of Satellite Oceanographic Data) altimetry data and the Regional Ocean Modeling System (ROMS) output data. A total of 10, 000 particles were released inside the warm eddy at 10, 50 and 100 m, respectively. The lifespan of the warm eddy was 121 days, with a mean radius of 50.4 km; and it traveled 1437.5 km at a mean speed of 13.5 cm·s-1. Most of the tracers were trapped inside the eddy and were carried southwestward along 1000-2000 m isobaths. Because of the terrain and its interaction with the flow, the eddy was more unstable during its terminal stage. Many of the tracers were expelled from the eddy, and the number of remaining tracers dropped to only 18.6%-35.6%. Although this ratio may seem small, the accumulative effects of transport were considerable. The number of tracers in the warm eddy had a strong positive correlation with potential vorticity (PV) with a correlation coefficient of 0.63. The tracers were trapped by the outmost PV contour The tracers inside the eddy sank in a spiral. Within the first 5 days, only 3.9% of the particles sank deeper than 15 m. The mean depth of tracer particles inside the eddy was observed to to 48.7, 88.7 and 130.6 m for those released at 10, 50 and 100 m, respectively.

Key words: northern South China Sea, southwest of Taiwan Island, warm eddy, particle transport, potential vorticity