Abstract
This study uses temperature and salinity time series acquired with taut-line moorings in the western equatorial Pacific to investigate water mass behavior on the thermocline layer. Basically, it is insufficient to trace water mass variation by the original discrete depth coordinate data because of relatively high variability of density at fixed depth near the thermocline. A reconstruction method based on the density surface motion caused by tidal forcing was used to derive continuous profiles of temperature and salinity from vertically discrete measurements at fixed depths. This method can represent detailed vertical salinity structures and their variation, especially along the potential density surface of 24.8σθ, where the salinity maximum of South Pacific tropical water (SPTW) appeared. Variability around the 24.8σθ surface at each site was as large as that observed at the surface, which suggests a strong influence of SPTW behavior. High salinity along the 24.8σθ surface within the equatorial band of the western Pacific appeared during boreal fall-winter at sites far from New Guinea. In contrast, high salinity appeared near New Guinea during the boreal spring-summer. These features suggest the influence of the New Guinea Coastal Undercurrent. Over longer time scales, several higher salinity events were observed. The most pronounced salinity event occurred during 2007–2008. Interannual variation of the salinity anomaly along the 24.8σθ surface was negatively correlated with the Niño 3.4 sea surface temperature anomaly. A long-term salinity anomaly shift from negative to positive occurred around the end of 2002. The relationship with decadal variation in subtropical cell transport is also discussed.
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References
Ando K, McPhaden MJ (1997) Variability of surface layer hydrography in the tropical Pacific Ocean. J Geophys Res 102:23063–23078
Ando K, Matsumoto T, Nagahama T, Ueki I, Takatsuki Y, Kuroda Y (2005) Drift characteristics of a moored conductivity-temperature-depth sensor and correction of salinity data. J Atmos Oceanic Technol 22:282–291
Antonov J, Levitus S, Boyer TP, Conkright M, O’Brien T, Stephens C (1998) World Ocean Atlas 1998 Vol. 2: Temperature of the Pacific Ocean. NOAA Atlas NESDIS 28, U.S. Gov Printing Office, Washington DC
Ashok K, Behera SK, Rao SA, Weng H, Yamagata T (2007) El Niño Modoki and its possible teleconnection. J Geophys Res 112: C11007. doi:10.1029/2006JC003798
Bosc C, Delcroix T, Maes C (2009) Barrier layer variability in the western Pacific warm pool from 2000 to 2007. J Geophys Res 114: C06023. doi:10.1029/2008JC005187
Boyer TP, Levitus S, Antonov J, Conkright M, O’Brien T, Stephens C (1998) World Ocean Atlas 1998 Vol. 5: Salinity of the Pacific Ocean. NOAA Atlas NESDIS 31, U.S. Gov Printing Office, Washington, DC
Delcroix T, Hénin C (1991) Seasonal and interannual variations of sea surface salinity in the tropical Pacific Ocean. J Geophys Res 96:22135–22150
Delcroix T, Hénin C, Porte V, Arkin P (1996) Precipitation and sea-surface salinity in the tropical Pacific Ocean. Deep Sea Res 43:1123–1141
Donguy JR (1994) Surface and subsurface salinity in the tropical Pacific Ocean: relations with climate. Prog Oceanogr 34:45–78
Feng M, Merrifield MA, Pinkel R, Hacker P, Plueddemann AJ, Firing E, Lukas R, Eriksen C (1998) Semidiurnal tides observed in the western equatorial Pacific during Tropical Ocean-Global Atmosphere. J Geophys Res 103:10253–10272
Fine RA, Lukas R, Bingham FM, Warner MJ, Gammon RH (1994) The western equatorial Pacific: a water mass crossroads. J Geophys Res 99:25063–25080
Gourdeau L (1998) Internal tides observed at 2°S-156°E by in situ and TOPEX/POSEIDON data during the Coupled Ocean-Atmosphere Response Experiment (COARE). J Geophys Res 103:12629–12638
Hasegawa T, Ando K, Ueki I, Mizuno K, Hosoda S (2013) Upper ocean salinity variability in the tropical Pacific: case study for quasi-decadal shift during 2000s using TRITON buoys and ARGO floats. J Clim (Accepted)
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
Johnson GC (2001) The Pacific Ocean subtropical cell surface limb. Geophys Res Lett 9:1771–1774
Johnson GC, McPhaden MJ (1999) Interior pycnocline flow from the subtropical to the equatorial Pacific Ocean. J Phys Oceanogr 29:3073–3089
Kantha LH, Tierney CC (1997) Global baroclinic tides. Prog Oceanogr 40:163–178
Kashino Y, Ueki I, Kuroda Y, Purwandani A (2007) Ocean variability north of New Guinea derived from TRITON buoy data. J Oceanogr 63:545–559
Kuroda Y (2000) Variability of currents off the northern coast of New Guinea. J Oceanogr 56:103–116
Kuroda Y, Amitani Y (2001) TRITON: new ocean and atmospheric observing buoy for monitoring ENSO. Umi no Kenkyu 10:157–172 (in Japanese with English abstract)
Lukas R, Lindstrom E (1991) The mixed layer of the western equatorial Pacific Ocean. J Geophys Res 96:3343–3357
Maes C (2000) Salinity variability in the equatorial Pacific Ocean during the 1993–98 period. Geophys Res Lett 27:1659–1662
Maes C, Belamari S (2011) On the impact of salinity barrier layer on the Pacific Ocean mean state and ENSO. SOLA 7:097–100. doi:10.2151/sola.2011-025
Maes C, Picaut J, Belamari S (2002a) Salinity barrier layer and onset of El Niño in a Pacific coupled model. Geophys Res Lett 29: 2206. doi:10.1029/2002GL016029
Maes C, McPhaden MJ, Behringer D (2002b) Signatures of salinity variability in tropical Pacific Ocean dynamic height anomalies. J Geophys Res 107. doi:10.1029/2000JC000737
Maes C, Picaut J, Belamari S (2005) Importance of the salinity barrier layer for the buildup of El Niño. J Clim 18:104–118
McPhaden MJ, Zhang D (2002) Slowdown of the meridional overturning circulation in the upper Pacific Ocean. Nature 415:603–608
McPhaden MJ, Zhang D (2004) Pacific Ocean circulation rebounds. Geophys Res Lett 31. doi:10.1029/2004GL020727
McPhaden MJ, Busalacchi AJ, Cheney R, Donguy JR, Gage KS, Halpern D, Ji M, Julian P, Meyers G, Mitchum GT, Niiler PP, Picaut J, Reynolds RW, Smith N, Takeuchi K (1998) The Tropical Ocean-Global Atmosphere (TOGA) observing system: a decade of progress. J Geophys Res 103:14169–14240
Niwa Y, Hibiya T (2001) Numerical study of the spatial distribution of the M2 internal tide in the Pacific Ocean. J Geophys Res 106:22441–22449
Schott FA, McCreary JP Jr, Johnson GC (2004) Shallow overturning circulations of the tropical-subtropical oceans. In: Wang C, Xie S-P, Carton JA (eds) Earth climate: the ocean-atmosphere interaction. AGU Geophys Monograph Series, vol 147, pp 261–304
Sprintall J, Tomczak M (1992) Evidence of the barrier layer in the surface layer of the Tropics. J Geophys Res 97:7305–7316
Tsuchiya M (1968) Upper waters of the intertropical Pacific Ocean. Johns Hopkins Oceanogr Stud, No. 4
Ueki I, Ando K, Kuroda Y, Kutsuwada K (2002) Salinity variation and its effect on dynamic height along the 156°E in the Pacific warm pool. Geophys Res Lett 29. doi:10.1029/2001GL013993
Ueki I, Kashino Y, Kuroda Y (2003) Observation of current variations off the New Guinea coast including the 1997–1998 El Niño period and their relationship with Sverdrup transport. J Geophys Res 108: 3243. doi:10.1029/2002JC001611
Zhang D, McPhaden MJ (2006) Decadal variability of the shallow Pacific meridional overturning circulation: relation to tropical sea surface temperatures in observations and climate change models. Ocean Modeling 15:250–273
Acknowledgments
We thank the members of the TRITON project. The TRITON moorings were deployed and recovered by R/V MIRAI, R/V KAIYO, and R/V YOKOSUKA. The TRITON project is supported by the Ministry of Education, Culture, Sports, Science and Technology, Japan. The authors acknowledge Dongxiao Zhang for the useful discussion about the decadal variation of STC transport. The Niño 3.4 SST anomaly data were downloaded from http://www.cpc.ncep.noaa.gov/data/indices/.
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Ueki, I., Ando, K. Detection of Pacific tropical water variability by taut-line moorings in the western equatorial Pacific. J Oceanogr 69, 429–441 (2013). https://doi.org/10.1007/s10872-013-0184-6
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DOI: https://doi.org/10.1007/s10872-013-0184-6