Interannual variability in the North Pacific meridional overturning circulation
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Abstract
We analyzed the temporal and spatial variation, and interannual variability of the North Pacific meridional overturning circulation using an empirical orthogonal function method, and calculated mass transport using Simple Ocean Data Assimilation Data from 1958–2008. The meridional streamfunction field in the North Pacific tilts N-S; the Tropical Cell (TC), Subtropical Cell (STC), and Deep Tropical Cell (DTC) may be in phase on an annual time scale; the TC and the STC are out of phase on an interannual time scale, but the interannual variability of the DTC is complex. The TC and STC interannual variability is associated with ENSO (El Niño-Southern Oscillation). The TC northward, southward, upward, and downward transports all weaken in El Niños and strengthen in La Niñas. The STC northward and southward transports are out of phase, while the STC northward and downward transports are in phase. Sea-surface water that reaches the middle latitude and is subducted may not completely return to the tropics. The zonal wind anomalies over the central North Pacific, which control Ekman transport, and the east-west slope of the sea level may be major factors causing the TC northward and southward transport interannual variability and the STC northward and southward transports on the interannual time scale. The DTC northward and southward transports decrease during strong El Niños and increase during strong La Niñas. DTC upward and downward transports are not strongly correlated with the Niño-3 index and may not be completely controlled by ENSO.
Keyword
North Pacific Ocean meridional overturning circulation interannual variation temporal and spatial variationsPreview
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References
- Capotondi A, Alexander M A. 2005. Anatorny and decadal evolution of the Pacific subtropical-tropical cells (STCs). J. Climate, 18: 3 739–3 758.CrossRefGoogle Scholar
- Gu D, Philander S G H. 1997. Interdecadal climate fluctuations that depend on exchanges between the tropics and extratropics. Science, 275: 805–807.CrossRefGoogle Scholar
- Izumo T. 2005. The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific Ocean. Ocean Dyn., 55: 110–123.CrossRefGoogle Scholar
- Kim Y Y, Qu T, Jensen T et al. 2004. Seasonal and interannual variations of the North Equatorial Current bifurcation in a high-resolution OGCM. J. Geophys. Res., 109: C03040, http://dx.doi.org/10.1029/2003JC002013.CrossRefGoogle Scholar
- Lee T, Fukumori I. 2003. Interannual-to-decadal variations of tropical-subtropial exchange in the Pacific Ocean: Boundary versus interior pycnocline transport. J. Climate, 16: 4 022–4 041.CrossRefGoogle Scholar
- Liu H, Zhang Q, Duan Y et al. 2011. The three-dimensional structure and seasonal variation of the North Pacific meridional overturning circulation. Acta Oceanol. Sin., 30(3): 33–42.CrossRefGoogle Scholar
- Liu Z, Philander S G H, Pacanowski R C. 1994. A GCM study of tropical-subtropical upper-ocean water ex-change. J. Phys. Oceanogr., 24: 2 606–2 623.Google Scholar
- Lohmann K, Latif M. 2005. Tropical Pacific decadal variability and the subtropical cells. J. Climate, 18: 5 163–5 178.CrossRefGoogle Scholar
- Lu P, McCreary J P, Klinger B A. 1998: Meridional circulation cells and the source waters of the Pacific equatorial undercurrent. J. Phys. Oceanogr., 28: 62–84.CrossRefGoogle Scholar
- McCreary J, Yu Z. 1992. Equatorial dynamics in the 2.5 layer model. Prog. Oceanogr., 29(1): 61–132.CrossRefGoogle Scholar
- McCreary J P, Lu P. 1994. Interaction between the subtropical and equatorial ocean circulations: The subtropical cell. J. Phys. Oceanogr., 24: 466–497.Google Scholar
- McPhaden M, Zhang D. 2002. Slowdown of the meridional overturning circulation in the upper Pacific Ocean. Nature, 415: 603–608.CrossRefGoogle Scholar
- McPhaden M, Zhang D. 2004. Pacific Ocean circulation rebounds. Geophys. Res. Lett., 31: L18301, http://dx.doi.org/10.1029/2004GL020727.CrossRefGoogle Scholar
- Nonaka M, Xie S, McCreary J P. 2001. Decadal variations in the subtropical cells and equatorial Pacific SST. Geophys. Res. Lett., 29(7): 1 116, http://dx.doi.org/10.1029/2001GL013-717.Google Scholar
- Pedlosky J. 1987. An inertial theory of the equatorial undercurrent. J. Phys. Oceanogr., 17: 1 978–1 985.Google Scholar
- Schott F A, Stramma L, Wang W, Giese B S, Zantopp R. 2008. Pacific subtropical cell variability in the SODA 2.0.2/3 assimilation. Geophys. Res. Lett., 35: L10607, http://dx.doi.org/10.1029/2008GL033757.CrossRefGoogle Scholar
- Wang Q, Huang R. 2005. Decadal variability of pycnocline flows from the subtropical to the Equatorial Pacific. J. Phys. Oceanogr., 35: 1 861–1 875.CrossRefGoogle Scholar
- Wyrtki K. 1975. El Niño—the dynamic response of the equatorial Pacific Ocean to atmosphere forcing. J. Phys. Oceanogr., 5: 572–583.CrossRefGoogle Scholar
- Zhang Q, Qi Q, Hou Y et al. 2007. Zonal displacement of the western Pacific Warm Pool and zonal wind anomaly over the Pacific Ocean. Chin. J. Oceanol. Limnol., 25(3): 277–285.CrossRefGoogle Scholar
- Zhang Q, Yang H, Zhong Y et al. 2005. An idealized study of the impact of extratropical climate change on El Niño-Southern Oscillation. Clim. Dynam., 25: 869–880.CrossRefGoogle Scholar