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Application of Empirical Orthogonal Function on Geodetic Time-Series Data

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dc.contributor.author Pasari, Sumanta
dc.date.accessioned 2023-08-14T09:34:39Z
dc.date.available 2023-08-14T09:34:39Z
dc.date.issued 2021
dc.identifier.uri https://ieeexplore.ieee.org/document/9792016
dc.identifier.uri http://dspace.bits-pilani.ac.in:8080/xmlui/handle/123456789/11383
dc.description.abstract Growing amount of geodetic data through sophisticated data collection techniques in recent times has led to substantial challenges in data analysis and interpretation. The empirical orthogonal function (EOF), commonly known as principal component analysis (PCA), is one of the dominant tools in analyzing coherent space-time dataset. The EOF method belongs to the family of factor analysis and has application in dimensionality reduction and pattern extraction, especially in the field of Geophysics, Atmospheric Sciences and Oceanography. This paper provides some basic formulation of the EOF technique with an emphasis on the step-by-step implementation to extract dominant modes from any time-series data. For instance, the EOF-based results show that the deformation pattern of the 2016, M w 7.8, Kaikoura earthquake of New Zealand is in the North-East direction. A few variations of the conventional EOF method are also discussed. en_US
dc.language.iso en en_US
dc.publisher IEEE en_US
dc.subject Mathematics en_US
dc.subject Time-series en_US
dc.subject Empirical Orthogonal Function (EOF) en_US
dc.subject Spatio-temporal analysis en_US
dc.title Application of Empirical Orthogonal Function on Geodetic Time-Series Data en_US
dc.type Article en_US


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