Variabilities of surface current in the tropical Pacific Ocean

Journal of Ocean University of Qingdao - Tập 1 - Trang 130-134 - 2002
Wang Qi1, Hu Ruijin1, Anna Zaklikowski2
1Department of Marine Meteorology, Ocean University of Qingdao, Qingdao, P.R. China
2Department of Civil and Environmental Engineering, Clarkson University, Potsdam, USA

Tóm tắt

The Simple Ocean Data Assimilation (SODA) package is used to better understand the variabilities of surface current transport in the Tropical Pacific Ocean from 1950 to 1999. Seasonal variation, internnual and decadal variability analyses are conducted on the three major surface currents of the Tropical Pacific Ocean: the North Equatorial Current (NEC), the North Equatorial Countecurrent (NECC), and the South Equatorial Current (SEC). The transport of SEC is quite larger than those of NEC and NECC. The SEC has two maximums in February and August. The NEC has a small annual variation. The NECC has a maximum in October and is very weak in March and April. All currents have remarkable interannual and decadal variabilities. The variabilities of the NEC and the SEC related to the winds over them well, but the relationship between the NECC and the wind over it is not close. Analysis related to El Niño-Southern Oscillation (ENSO) suggests that before El Niño (La Niña) the SEC is weaker (stronger) and the NECC is stronger (weaker), after El Niño (La Niña) the SEC is stronger (weaker) and the SEC is weaker (stronger). There is no notable relationship between the NEC and ENSO.

Tài liệu tham khảo

Catos-Figuerola, A., and B. A. Taft, 1983. The South Equatorial Current during the 1979–80 Hawaii-Tahiti Shuttle. Tropical Ocean-Atmosphere Newsletter, 9, 6–8. Carton, J. A., G. Chepurin, Cao, X., and B. S. Giese, 1999. A simple ocean data assimilation analysis of the global upper ocean 1950–1995, part 1: methodology. J. Phys. Oceanogr., 30: 294–309. Donguy, J. R., and G. Meyers, 1996. Mean annual variation of transport of major currents in the Tropical Pacific Ocean. Deep-Sea Res., 43 (7): 1105–1122. Harrisson D. E., W. S. Kessler, and B. S. Giese, 1989. Ocean circulation model hindcasts of the 1982–1983 El Niño: thermal variability along the ship-of-opportunity tracks. J. Phys. Oceanogr., 19: 397–418. McPhaden, M. J., A. J. Busalacchi, and J. Picaut, 1988. Observations and wind-forced model simulations of the means seasonal cycle in tropical Pacific sea surface topography. J. Geosphys. Res., 93 (c7): 8131–8146. Meyers, G., and J. R. Donguy, 1984. The North Equatorial Countercurrent and heat Storage in the western Pacific Ocean during 1982–83. Nature, 5991: 258–260. Talley, L. D., G. Fryer, and R. Lumpkin, 1998. Physical oceanography of the Tropical Pacific, Geography of the Pacific Islands. Bess Press, pp. 19–32. Wyrtki, K, and B. Kilonsky, 1984. Mean water and current structure during the Hawaii-Tahiti Shuttle Experiment. J. Phys. Oceanogr., 14: 242–254.