POLAR MOTIONS WITH A HALF-CHANDLER PERIOD AND LESS IN THEIR TEMPORAL VARIABILITY

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dc.contributor.author Hopfner J.
dc.date.accessioned 2021-12-28T06:33:23Z
dc.date.available 2021-12-28T06:33:23Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=4699478
dc.identifier.citation Journal of Geodynamics, 2003, 36, 3, 407-422
dc.identifier.issn 0264-3707
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/33876
dc.description.abstract Our study focuses on the observed higher-frequency polar motions that are substantially smaller than the Chandler and annual wobbles. Here, the combined Earth orientation series SPACE99 from 1976 to 2000 with one-day sampling is used as input data, after removing the low-frequency, the Chandler and annual terms. We applied a data processing procedure including four steps, each computing the amplitude spectrum by a Fast Fourier Transform in order to reveal the periodic signals in the residual motions, and then separating their components from the residual time series by band-pass filtering. In particular, the oscillations have the following periods: semi-Chandler and semi-annual periods and those of order four, three, two, and one and a half months, as well as quasi-biennial and 300-day periods. We show to what extent the observed polar motions are irregularly occurring. A very small polar motion signal with the period of one month is still found in the remaining motions.
dc.subject POLAR MOTION
dc.subject PERIODIC COMPONENTS
dc.subject SEMI-CHANDLER WOBBLE
dc.subject SEMI-ANNUAL WOBBLE, AND 4-MONTH, 90-DAY, 2-MONTH AND 1.5-MONTH COMPONENTS
dc.subject QUASI-BIENNIAL AND 300-DAY COMPONENTS
dc.subject MAGNITUDE
dc.subject VARIABILITY
dc.title POLAR MOTIONS WITH A HALF-CHANDLER PERIOD AND LESS IN THEIR TEMPORAL VARIABILITY
dc.type Статья


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