Barrier Layer and Relevant Variability of the Salinity Field in the Equatorial Pacific Estimated in an Ocean Reanalysis Experiment

• Published in: Pure and applied geophysics Vol. 169; no. 3; pp. 579 - 594
• Main Authors: Fujii, Y., Kamachi, M., Matsumoto, S., Ishizaki, S.
• Format: Journal Article
• Language: English
• Published: Basel SP Birkhäuser Verlag Basel 01.03.2012; Springer Nature B.V
• Subjects: Assimilation; Barrier layers; Buoys; Data assimilation; Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; Oceanic analysis; Oceans; Oscillations; Salinity; Statistics; Variables; IS, Equatorial Pacific; Barrier Layer; High Salinity Water; Salinity Field; Empirical Orthogonal Function Mode; Mixed Layer Depth
• ISSN: 0033-4553; 1420-9136
• DOI: 10.1007/s00024-011-0387-y

This paper investigates the feasibility of an ocean data assimilation system to analyze the salinity variability associated with the barrier layer in the equatorial Pacific. In order to validate reproducibility of the temperature and salinity fields, we perform an assimilation run where some temperature and salinity observations by TRITON buoys and Argo floats are withheld. The assimilation run reproduces interannual variability of salinity in the equatorial Pacific exhibited in the data that are withheld. Statistics shows that salinity values and variations in the assimilation run are closer to the data than the climatology and in the model free run. We also confirm that zonal currents in the equatorial Pacific in the reanalysis, where all available temperature and salinity data are assimilated, are consistent with an observation-based mapping and the data of the Acoustic Doppler Current Profiler mounted on TAO buoys. Variability of the barrier layer and relevant salinity field in the reanalysis is consistent with former studies. A thick barrier layer area generally exists west of the equatorial salinity front and is displaced zonally with the migration of the front in the response to El Niño-Southern Oscillation, although the area moved to the east over the front in the 1997 El Niño. It is confirmed that the barrier layer thickness is closely correlated with the near-surface temperature in the equatorial Pacific.