Abstract
The origins and evolutions of two anticyclonic eddies in the northeastern South China Sea (SCS) were examined using multi-satellite remote sensing data, trajectory data of surface drifting buoys, and in-situ hydrographic data during winter 2003/2004. The results showed that buoy 22918 tracked an anti-cyclonic warm-core eddy (AE1) for about 20 days (December 4–23, 2003) in the northeastern SCS, and then escaped from AE1 eventually. Subsequently to that, buoy 22517 remained within a different anti-cyclonic warm-core eddy (AE2) for about 78 days (from January 28 to April 14, 2004) in the same area. It drifted southwestward for about 540 km, and finally entered into the so-called “Luzon Gyre”. Using inference from sea level anomaly (SLA), sea surface temperature (SST), geostrophic currents and the buoys’ trajectories, it is shown that both eddies propagated southwestward along the continental slope of the northern SCS. The mean speeds of AE1 and AE2 movements were 9.7 cm/s and 10.5 cm/s, respectively, which are similar to the phase speed of Rossby waves in the northern SCS. The variation of instantaneous speeds of the eddy movement and intensity of anticyclonic eddy may suggest complex interactions between an anticyclonic eddy and its ambient fluids in the northern SCS, where the eddy propagated southwestward with Rossby waves. Furthermore, SLA and SST images in combination with the temperature and salinity profiles obtained during a cruise suggested that AE1 was generated in the interior SCS and AE2 was shed from the “Kuroshio meander”.
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Caruso, M. J., G. G. Gawarkiewicz and R. C. Beardsley (2006): Interannual variability of the Kuroshio intrusion in the South China Sea. J. Oceanogr., 62, 559–575.
Centurioni, L. R., P. P. Niiler and D.-K. Lee (2004): Observation of inflow of Philippine Sea surface water into the South China Sea through the Luzon Strait. J. Phys. Oceanogr., 34, 113–121.
Guan, B. and Y. Yuan (2006): Overview of studies on some eddies in the South China Seas and their adjacent seas, I. The South China Sea and the region east of Taiwan. Acta Oceanol. Sinica, 28(3), 1–16 (in Chinese with English abstract).
He, Z. G., D. Wang and J. Y. Hu (2002): Features of eddy kinetic energy and variations of upper circulation in the South China Sea. Acta Oceanol. Sinica, 21(2), 305–314.
Hetland, R. H., Y. Hsueh, R. R. Leben and P. P. Niiler (1999): A loop current-induced jet along the edge of the West Florida shelf. Geophys. Res. Lett., 26(15), 2239–2242.
Hu, J., H. Kawamura, H. Hong, F. Kobashi and D. Wang (2001): 3–6 months variation of sea surface height in the South China Sea and its adjacent ocean. J. Oceanogr., 57, 69–78.
Huang, Q. and Y. Zheng (1996): Currents in the northeastern South China Sea and Bashi Channel in March, 1992. Oceanogr. China, 6, 42–51 (in Chinese with English abstract).
Hurlburt, H. E. and J. D. Thompson (1980): A numerical study of loop current intrusions and eddy shedding. J. Phys. Oceanogr., 10, 1611–1651.
Isern-Fontanet, J., E. García-Ladona and J. Font (2002): Identification of marine eddied from altimetric maps. J. Atmos. Oceanic Technol., 20, 772–778.
Jia, Y. and Q. Liu (2004): Eddy shedding from the Kuroshio bend at Luzon Strait. J. Oceanogr., 60(6), 1063–1069.
Jia, Y., Q. Liu and W. Liu (2005): Primary studies of the mechanism of eddy shedding from the Kuroshio bend in Luzon Strait. J. Oceanogr., 61(6), 1017–1027.
Kennan, S. C. and P. J. Flament (2000): Observation of a tropical instability vortex. J. Phys. Oceanogr., 30, 2277–2301.
Li, L. and B. Wu (1989): A Kuroshio loop in South China Sea? J. Oceanogr. Taiwan Strait, 8, 89–95 (in Chinese with English abstract).
Li, L., W. D. Nowlin, Jr. and J.-L. Su (1998): Anticyclonic rings from the Kuroshio in the South China Sea. Deep-Sea Res., Part I, 45, 1469–1482.
Li, Y., L. Li, M. Lin and W. Cai (2002): Observation of mesoscale eddy fields in the sea southwest of Taiwan by TOPEX/Poseidon altimeter data. Acta Oceanol. Sinica, 24, 163–170 (in Chinese with English abstract).
Metzger, E. J. and H. E. Hurlburt (2001): The nondeterministic nature of Kuroshio penetration and eddy shedding in the South China Sea. J. Phys. Oceanogr., 31, 1712–1732.
Nof, D. (1981): On the β-induced movement of isolated baroclinic eddies. J. Phys. Oceanogr., 11, 1662–1672.
Nof, D. (1988): The fusion of isolated nonlinear eddies. J. Phys. Oceanogr., 18, 887–905.
Nowlin, W. D., Jr, J. M. Hubertz and R. Q. Reid (1968): A detached eddy in the Gulf of Mexico. J. Mar. Res., 26, 185–186.
Qu, T. (2000): Upper-layer circulation in the South China Sea. J. Phys. Oceanogr., 30, 1450–1460.
Qu, T. (2001): Role of ocean dynamics in determining the mean seasonal cycle of the South China Sea surface temperature. J. Geophys. Res., 106(C4), 6943–6955.
Qu, T., H. Misudera and T. Yamagata (2000): Intrusion of the North Pacific waters into the South China Sea. J. Geophys. Res., 105(C3), 6415–6424.
Sangrà, P., J. L. Pelegrì, A. Hernàndez-Guerra, I. Arregui, J. M. Martìn, A. Marrero-Dìaz, A. Martìnez, A. W. Ratsimandresy and A. Rodríguez-Santana (2005): Life history of an anticyclone eddy. J. Geophys. Res., 110, C03021, doi:10.1029/2004JC002526.
Shaw, P. T. (1989): The intrusion of water masses into the sea of southwest of Taiwan. J. Geophys. Res., 94, 18213–18226.
Shaw, P. T. (1991): The seasonal variation of the intrusion of the Philippine Sea into the South China Sea. J. Geophys. Res., 96, 821–827.
Soong, Y. S., J. H. Hu, C. R. Ho and P. P. Niiler (1995): Cold-core eddy detected in South China Sea. EOS Trans. AGU, 76, 345–347.
Sturges, W. (1994): The frequency of ring separation from the Loop Current. J. Phys. Oceanogr., 24, 1647–1651.
Su, J. (2004): Overview of the South China Sea cuirculation and its influene on the coatal physical oceanography outside the Pearl River Estuary. Deep-Sea Res., 24, 1745–1760.
Su, J. (2005): Overview of the South China Sea circulation and its dynamics. Acta Oceanol. Sinica, 27(6), 1–8 (in Chinese with English abstract).
Su, J., J. Lu, Y. Hou, G. Fang, Z. Wei and B. Yin (2002): Analysis of satellite-tracked drifting buoys in the South China Sea. Oceanol. Limnol. Sinica, 33(2), 121–127 (in Chinese with English abstract).
Wang, G., J. Su and P. C. Chu (2003): Mesoscale eddies in the South China Sea observed with altimeter data. Geophys. Res. Lett., 30(21), 2121, doi:10.1029/2003GL018532.
Wang, J. and C.-S. Chern (1987): The warm-core eddy in the northern South China Sea. I. Preliminary observations on the warm-core eddy. Acta Oceanogr. Taiwan., 18, 92–103 (in Chinese with English abstract).
Wang, L., C. J. Koblinsky and S. Howden (2000): Mesoscale variability in the South China Sea from the TOPEX/Poseidon altimetry data. Deep-Sea Res., Part I, 47, 681–708.
White, W. B. (2000): Tropic coupled Rossby waves in the Pacific ocean-atmosphere system. J. Phys. Oceanogr., 30(6), 1245–1264.
Wyrtki, K. (1961): Physical oceanography of the Southeast Asian waters. Naga Rep., 2, 1–195 pp.
Yang, K., P. Shi, D. Wang and Y. Qi (2000): Numerical study about the mesoscale multi-eddy system in the northern South China Sea in winter. Acta Oceanol. Sinica, 22(1), 27–34 (in Chinese with English abstract).
Yuan, D., W. Han and D. Hu (2006): Surface Kuroshio path in the Luzon Strait area derived from satellite remote sensing data. J. Geophys. Res., 111, C11007, doi:10.1029/2005JC003412.
Yuan, D., W. Han and D. Hu (2007): Anti-cyclonic eddies northwest of Luzon in summer-fall observed by satellite altimeters. Geophys. Res. Lett., 34, L13610, doi:10.1029/2007GL029401.
Yuan, S. Y. and Z. Z. Wang (1986): Topography forced Rossby waves in the section from Xisha to Dongsha Islands. Trop. Oceanol., 5(3), 1–6 (in Chinese with English abstract).
Yuan, Y., X. Bu, G. Liao, R. Luo, J. Su and K. Wang (2004): Diagnostic calculation of the upper-layer circulation in the South China Sea during the winter of 1998. Acta Oceanol. Sinica, 23(2), 187–199.
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Wang, D., Xu, H., Lin, J. et al. Anticyclonic eddies in the northeastern South China Sea during winter 2003/2004. J Oceanogr 64, 925–935 (2008). https://doi.org/10.1007/s10872-008-0076-3
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DOI: https://doi.org/10.1007/s10872-008-0076-3