New significance test methods for Fourier analysis of geophysical time series

When one applies the discrete Fourier transform to analyze finite-length time series, discontinuities at the data boundaries will distort its Fourier power spectrum. In this paper, based on a rigid statistics framework, we present a new significance test method which can extract the intrinsic featur...

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Published in:Nonlinear Processes in Geophysics
Main Authors: Zhang, Z., Moore, J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/npg-18-643-2011
https://npg.copernicus.org/articles/18/643/2011/
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spelling ftcopernicus:oai:publications.copernicus.org:npg11288 2023-05-15T15:00:07+02:00 New significance test methods for Fourier analysis of geophysical time series Zhang, Z. Moore, J. 2018-01-15 application/pdf https://doi.org/10.5194/npg-18-643-2011 https://npg.copernicus.org/articles/18/643/2011/ eng eng doi:10.5194/npg-18-643-2011 https://npg.copernicus.org/articles/18/643/2011/ eISSN: 1607-7946 Text 2018 ftcopernicus https://doi.org/10.5194/npg-18-643-2011 2020-07-20T16:26:01Z When one applies the discrete Fourier transform to analyze finite-length time series, discontinuities at the data boundaries will distort its Fourier power spectrum. In this paper, based on a rigid statistics framework, we present a new significance test method which can extract the intrinsic feature of a geophysical time series very well. We show the difference in significance level compared with traditional Fourier tests by analyzing the Arctic Oscillation (AO) and the Nino3.4 time series. In the AO, we find significant peaks at about 2.8, 4.3, and 5.7 yr periods and in Nino3.4 at about 12 yr period in tests against red noise. These peaks are not significant in traditional tests. Text Arctic Copernicus Publications: E-Journals Arctic Nonlinear Processes in Geophysics 18 5 643 652
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description When one applies the discrete Fourier transform to analyze finite-length time series, discontinuities at the data boundaries will distort its Fourier power spectrum. In this paper, based on a rigid statistics framework, we present a new significance test method which can extract the intrinsic feature of a geophysical time series very well. We show the difference in significance level compared with traditional Fourier tests by analyzing the Arctic Oscillation (AO) and the Nino3.4 time series. In the AO, we find significant peaks at about 2.8, 4.3, and 5.7 yr periods and in Nino3.4 at about 12 yr period in tests against red noise. These peaks are not significant in traditional tests.
format Text
author Zhang, Z.
Moore, J.
spellingShingle Zhang, Z.
Moore, J.
New significance test methods for Fourier analysis of geophysical time series
author_facet Zhang, Z.
Moore, J.
author_sort Zhang, Z.
title New significance test methods for Fourier analysis of geophysical time series
title_short New significance test methods for Fourier analysis of geophysical time series
title_full New significance test methods for Fourier analysis of geophysical time series
title_fullStr New significance test methods for Fourier analysis of geophysical time series
title_full_unstemmed New significance test methods for Fourier analysis of geophysical time series
title_sort new significance test methods for fourier analysis of geophysical time series
publishDate 2018
url https://doi.org/10.5194/npg-18-643-2011
https://npg.copernicus.org/articles/18/643/2011/
geographic Arctic
geographic_facet Arctic
genre Arctic
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op_source eISSN: 1607-7946
op_relation doi:10.5194/npg-18-643-2011
https://npg.copernicus.org/articles/18/643/2011/
op_doi https://doi.org/10.5194/npg-18-643-2011
container_title Nonlinear Processes in Geophysics
container_volume 18
container_issue 5
container_start_page 643
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