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Variability in Solomon Sea circulation derived from altimeter sea level data
Melet A., Gourdeau L., Verron J.
Ocean Dynamics 60, 4 (2010) 883-900 - http://hal.archives-ouvertes.fr/hal-00534038
Articles dans des revues avec comité de lecture
Planète et Univers/Sciences de la Terre/Océanographie
Variability in Solomon Sea circulation derived from altimeter sea level data
Angélique Melet 1, Lionel Gourdeau 2, Jacques Verron () 1
1 :  Laboratoire des écoulements géophysiques et industriels (LEGI)
http://www.legi.grenoble-inp.fr/
CNRS : UMR5519 – Université Joseph Fourier - Grenoble I – Institut polytechnique de Grenoble (Grenoble INP)
1025 Rue de la piscine - BP 53 38041 GRENOBLE CEDEX 9
France
2 :  Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
http://www.legos.obs-mip.fr/
CNRS : UMR5566 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
14 avenue Edouard Belin 31400 Toulouse
France
OLVAC
The Solomon Sea is a key region in the Pacific Ocean where equatorial and subtropical circulations are connected. The region exhibits the highest levels in sea level variability in the entire south tropical Pacific Ocean. Altimeter data was utilized to explore sea level and western boundary currents in this poorly understood portion of the ocean. Since the geography of the region is extremely intricate, with numerous islands and complex bathymetry, specifically reprocessed along-track data in addition to standard gridded data were utilized in this study. Sea level anomalies (SLA) in the Solomon Sea principally evolve at seasonal and interannual time scales. The annual cycle is phased by Rossby waves arriving in the Solomon Strait, whereas the interannual signature corresponds to the basin-scale ENSO mode. The highest SLA variability are concentrated in the eastern Solomon Sea, particularly at the mouth of the Solomon Strait, where they are associated with a high eddy kinetic energy signal that was particularly active during the phase transition during the 1997-1998 ENSO event. Track data appear especially helpful for documenting the fine structure of surface coastal currents. The annual variability of the boundary currents that emerged from altimetry compared quite well with the variability seen at the thermocline level, as based on numerical simulations. At interannual time scales, western boundary current transport anomalies counterbalance changes in western equatorial Pacific warm water volume, confirming the phasing of South Pacific western boundary currents to ENSO. Altimetry appears to be a valuable source of information for variability in low latitude western boundary currents and their associated transport in the South Pacific.
Anglais

Ocean Dynamics
Publisher Springer Verlag (Germany)
ISSN 1616-7341 (eISSN : 1616-7228)
internationale
2010
60
4
883-900