Please use this identifier to cite or link to this item: https://doi.org/10.3989/scimar.04691.05A
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dc.titleLong-term regional trend and variability of mean sea level during the satellite altimetry era [Tendencia regional a largo plazo y variabilidad del nivel medio del mar en la era de la altimetría por satelite]
dc.contributor.authorLuu, Q.-H.
dc.contributor.authorWu, Q.
dc.contributor.authorTkalich, P.
dc.contributor.authorChen, G.
dc.date.accessioned2021-11-16T07:25:42Z
dc.date.available2021-11-16T07:25:42Z
dc.date.issued2019
dc.identifier.citationLuu, Q.-H., Wu, Q., Tkalich, P., Chen, G. (2019). Long-term regional trend and variability of mean sea level during the satellite altimetry era [Tendencia regional a largo plazo y variabilidad del nivel medio del mar en la era de la altimetría por satelite]. Scientia Marina 83 (2) : 111-120. ScholarBank@NUS Repository. https://doi.org/10.3989/scimar.04691.05A
dc.identifier.issn0214-8358
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/206405
dc.description.abstractSummary: The rise and fall of mean sea level are non-uniform around the global oceans. Their long-term regional trend and variability are intimately linked to the fluctuations and changes in the climate system. In this study, geographical patterns of sea level change derived from altimetric data over the period 1993-2015 were partitioned into large-scale oscillations allied with prevailing climatic factors after an empirical orthogonal function analysis. Taking into account the El Niño–Southern Oscillation (ENSO) and the Pacific Decadal Oscillations (PDO), the sea level change deduced from the multiple regression showed a better estimate than the simple linear regression thanks to significantly larger coefficients of determination and narrower confidence intervals. Regional patterns associated with climatic factors varied greatly in different basins, notably in the eastern and western regions of the Pacific Ocean. The PDO exhibited a stronger impact on long-term spatial change in mean sea level than the ENSO in various parts of the Indian and Pacific Oceans, as well as of the subtropics and along the equator. Further improvements in the signal decomposition technique and physical understanding of the climate system are needed to better attain the signature of climatic factors on regional mean sea level. © 2019 CSIC.
dc.publisherCSIC Consejo Superior de Investigaciones Cientificas
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceScopus OA2019
dc.subjectClimate variability
dc.subjectEl Niño-Southern oscillation
dc.subjectPacific decadal oscillations
dc.subjectRegional sea level trend
dc.subjectSea level rise
dc.typeArticle
dc.contributor.departmentTROPICAL MARINE SCIENCE INSTITUTE
dc.description.doi10.3989/scimar.04691.05A
dc.description.sourcetitleScientia Marina
dc.description.volume83
dc.description.issue2
dc.description.page111-120
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