WAVELET COHERENCE ANALYSIS OF LENGTH-OF-DAY VARIATIONS AND EL NIñO-SOUTHERN OSCILLATION

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dc.contributor.author Liu L.T.
dc.contributor.author Hsu H.T.
dc.contributor.author Grafarend E.W.
dc.date.accessioned 2023-12-16T06:35:07Z
dc.date.available 2023-12-16T06:35:07Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=28011325
dc.identifier.citation Journal of Geodynamics, 2005, 39, 3, 267-275
dc.identifier.issn 0264-3707
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/42342
dc.description.abstract Wavelet coherence analysis is defined and used to analyze the relationships between Length-Of-Day (LOD) variations and El Niño-Southern Oscillation (ENSO) on interannual scales. Using the newest observation data, this study quantitatively shows time-scale- dependent correlations and phase shifts between LOD variations and the ENSO. Good no-lag correlations (larger than 0.8) can be found on 3.0-4.9-year scales, while either obvious phase-shifts or low correlations are found on the other interannual scales. Around 2.5-year (biennial), 3.5-year and 5.0-year scales (i.e. around the time scales of ENSO's significant modes), the LOD variations with respect to the ENSO lag in phase by 4-5 months, lead by 3 months and lag by 3-5 months, respectively. Thus, there are obvious time-scale-dependent correlations and phase-shifts between the Earth rotation rate variations and the ENSO even within interannual scales. © 2005 Elsevier Ltd. All rights reserved.
dc.subject EL NIñO-SOUTHERN OSCILLATION
dc.subject LENGTH-OF-DAY VARIATIONS
dc.subject WAVELET COHERENCE ANALYSIS
dc.title WAVELET COHERENCE ANALYSIS OF LENGTH-OF-DAY VARIATIONS AND EL NIñO-SOUTHERN OSCILLATION
dc.type Статья
dc.identifier.doi 10.1016/j.jog.2004.11.003


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