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The seasonal march of the equatorial Pacific upper-ocean and its El Nino variability

TitleThe seasonal march of the equatorial Pacific upper-ocean and its El Nino variability
Publication TypeJournal Article
Year of Publication2017
AuthorsGasparin F., Roemmich D.
JournalProgress in Oceanography
Date Published2017/08
Type of ArticleArticle
ISBN Number0079-6611
Accession NumberWOS:000411770600001
Keywordsannual cycle; annual rossby-wave; boreal winter; eastern-pacific; layer; phase-locking; salinity; sea-surface temperature; tropical pacific; warm pool; westerly wind bursts

Based on two modern data sets, the climatological seasonal march of the upper-ocean is examined in the equatorial Pacific for the period 2004-2014, because of its large contribution to the total variance, its relationship to El Nino, and its unique equatorial wave phenomena. Argo provides a broadscale view of the equatorial Pacific upper-ocean based on subsurface temperature and salinity measurements for the period 2004-2015, and satellite altimetry provides synoptic observations of the sea surface height (SSH) for the period 1993-2015. Using either 11-year (1993-2003/2004-2014) time-series for averaging, the seasonal Rossby waves stands out clearly and eastward intraseasonal Kelvin wave propagation is strong enough in individual years to leave residuals in the 11-year averages, particularly but not exclusively, during El Nino onset years. The agreement of altimetric SSH minus Argo steric height (SH) residuals with GRACE ocean mass estimates confirms the scale-matching of in situ variability with that of satellite observations. Surface layer and subsurface thermohaline variations are both important in determining SH and SSH basin-wide patterns. The SH/SSH October-November maximum in the central-eastern Pacific is primarily due to a downward deflection of the thermocline (similar to 20 m), causing a warm subsurface anomaly (>1 degrees C), in response to the phasing of downwelling intraseasonal Kelvin and seasonal Rossby waves. Compared with the climatology, the stronger October-November maximum in the 2004-2014 El Nino composites is due to higher intraseasonal oscillations and interannual variability. Associated with these equatorial wave patterns along the thermocline, the western warm/fresh pool waters move zonally at interannual timescales through zonal wind stress and pressure gradient fluctuations, and cause substantial fresh (up to 0.6 psu) and warm (similar to 1 degrees C higher than the climatology) anomalies in the western central Pacific surface-layer during the El Nino onset year, and of the opposite sign during the termination year. These El Nino-related patterns are then analyzed focusing on the case of the onset of the strong 2015/2016 episode, and are seen to be around two times larger than that in the 2004-2014 El Nino composites. The present work exploits the capabilities of Argo and altimetry to update and improve the description of the physical state of the equatorial Pacific upper-ocean, and provides a benchmark for assessing the accuracy of models in representing equatorial Pacific variability. (C) 2017 Elsevier Ltd. All rights reserved.

Short TitleProg. Oceanogr.
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