Cite this paper:
MA Xiao, SUN Che. Equatorward shift of annual Rossby waves in the Equatorial Pacifi c Ocean[J]. Journal of Oceanology and Limnology, 2016, 34(1): 212-218

Equatorward shift of annual Rossby waves in the Equatorial Pacifi c Ocean

MA Xiao1,2, SUN Che1,
1 Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2 University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:
Annual Rossby wave is a key component of the ENSO phenomenon in the equatorial Pacifi c Ocean. Due to the paucity and seasonal bias in historical hydrographic data, previous studies on equatorial Rossby waves only gave qualitative description. The accumulation of Argo measurements in recent years has greatly alleviated the data problem. In this study, seasonal variation of the equatorial Pacifi c Ocean is examined with annual harmonic analysis of Argo gridded data. Results show that strong seasonal signal is present in the western equatorial Pacifi c and explains more than 50% of the thermal variance below 500 m. Lag-correlation tracing further shows that this sub-thermocline seasonal signal originates from the eastern equatorial Pacifi c via downward and southwestward propagation of annual Rossby waves. Possible mechanisms for the equatorward shift of Rossby wave path are also discussed.
Key words:    equatorial Pacifi c|annual Rossby wave|equatorward shift|Argo profi les|MOAA-GPV gridded data   
Received: 2015-01-13   Revised: 2015-03-02
Tools
PDF (1653 KB) Free
Print this page
Add to favorites
Email this article to others
Authors
Articles by MA Xiao
Articles by SUN Che
References:
Bosc C, Delcroix T. 2008. Observed equatorial Rossby waves and ENSO-related warm water volume changes in the equatorial Pacifi c Ocean. J. Geophys. Res ., 113 (C6):C06003, http://dx.doi.org/10.1029/2007JC004613.
Busalacchi A J, O’Brien J J. 1980. The seasonal variability in a model of the tropical Pacifi c. J. Phys. Oceanogr ., 10 (12): 1 929-1 951.
Challenor P G, Cipollini P, Cromwell D. 2001. Use of the 3D Radon transform to examine the properties of oceanic Rossby waves. J. Atmos. Oceanic Technol ., 18 (9): 1 558- 1 566.
Durland T S, Samelson R M, Chelton D B, de Szoeke R A. 2011. Modifi cation of long equatorial Rossby wave phase speeds by zonal currents. J. Phys. Oceanogr ., 41 (6): 1 077-1 101.
Hosoda S, Ohira T, Nakamura T. 2008. A monthly mean dataset of global oceanic temperature and salinity derived from Argo fl oat observations. In : JAMSTEC Report of Research and Development, Vol. 8. Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan. p.47-59.
Kessler W S, McCreary J P. 1993. The annual wind-driven Rossby wave in the subthermocline equatorial Pacifi c. J .Phys. Oceanogr ., 23 (6): 1 192-1 207.
Kessler W S. 2006. The circulation of the eastern tropical Pacifi c: A review. Prog. Oceanogr ., 69 (2-4): 181-217.
Lukas R, Firing E. 1985. The annual Rossby wave in the central equatorial Pacifi c Ocean. J. Phys. Oceanogr ., 15 (1): 55-67.
Marin F, Kestenare E, Delcroix T et al. 2010. Annual reversal of the equatorial intermediate current in the Pacifi c: observations and model diagnostics. J. Phys. Oceanogr ., 40 (5): 915-933.
Meyers G. 1979. On the annual Rossby wave in the tropical North Pacifi c Ocean. J. Phys. Oceanogr ., 9 (4): 663-674.
Perez R C, Chelton D B, Miller R N. 2005. The eff ects of wind forcing and background mean currents on the latitudinal structure of equatorial Rossby waves. J. Phys. Oceanogr ., 35 (5): 666-682.
Philander S G H. 1979. Equatorial waves in the presence of the equatorial undercurrent. J. Phys. Oceanogr ., 9 (2): 254-262.
Proehl J A. 1990. Equatorial wave-mean fl ow interaction: The long Rossby waves. J. Phys. Oceanogr ., 20 (2): 274-294.
Qu T D, Gan J P, Ishida A et al. 2008. Semiannual variation in the western tropical Pacifi c Ocean. Geophys. Res. Lett ., 35 (16): L16602, http://dx.doi.org/10.1029/2008GL035058.
Yu X R, McPhaden M. 1999. Seasonal variability in the equatorial Pacifi c. J. Phys. Oceanogr ., 29 (5): 925-947.
Copyright © Haiyang Xuebao