On studying relations between time series in climatology

Relationships between time series are often studied on the basis of cross-correlation coefficients and regression equations. This approach is generally incorrect for time series, irrespective of the cross-correlation coefficient value, because relations between time series are frequency-dependent. M...

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Main Author: V. Privalsky
Format: Article
Language:English
Published: Copernicus Publications 2015-06-01
Series:Earth System Dynamics
Online Access:http://www.earth-syst-dynam.net/6/389/2015/esd-6-389-2015.pdf
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spelling doaj-d7ee47e2b6be4ab8b82ea90864a03f492020-11-24T22:39:28ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872015-06-016138939710.5194/esd-6-389-2015On studying relations between time series in climatologyV. Privalsky0Space Dynamics Laboratory, Logan, Utah, USARelationships between time series are often studied on the basis of cross-correlation coefficients and regression equations. This approach is generally incorrect for time series, irrespective of the cross-correlation coefficient value, because relations between time series are frequency-dependent. Multivariate time series should be analyzed in both time and frequency domains, including fitting a parametric (preferably, autoregressive) stochastic difference equation to the time series and then calculating functions of frequency such as spectra and coherent spectra, coherences, and frequency response functions. The example with a bivariate time series "Atlantic Multidecadal Oscillation (AMO) – sea surface temperature in Niño area 3.4 (SST3.4)" proves that even when the cross correlation is low, the time series' components can be closely related to each other. A full time and frequency domain description of this bivariate time series is given. The AMO–SST3.4 time series is shown to form a closed-feedback loop system with a 2-year memory. The coherence between AMO and SST3.4 is statistically significant at intermediate frequencies where the coherent spectra amount up to 55 % of the total spectral densities. The gain factors are also described. Some recommendations are offered regarding time series analysis in climatology.http://www.earth-syst-dynam.net/6/389/2015/esd-6-389-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. Privalsky
spellingShingle V. Privalsky
On studying relations between time series in climatology
Earth System Dynamics
author_facet V. Privalsky
author_sort V. Privalsky
title On studying relations between time series in climatology
title_short On studying relations between time series in climatology
title_full On studying relations between time series in climatology
title_fullStr On studying relations between time series in climatology
title_full_unstemmed On studying relations between time series in climatology
title_sort on studying relations between time series in climatology
publisher Copernicus Publications
series Earth System Dynamics
issn 2190-4979
2190-4987
publishDate 2015-06-01
description Relationships between time series are often studied on the basis of cross-correlation coefficients and regression equations. This approach is generally incorrect for time series, irrespective of the cross-correlation coefficient value, because relations between time series are frequency-dependent. Multivariate time series should be analyzed in both time and frequency domains, including fitting a parametric (preferably, autoregressive) stochastic difference equation to the time series and then calculating functions of frequency such as spectra and coherent spectra, coherences, and frequency response functions. The example with a bivariate time series "Atlantic Multidecadal Oscillation (AMO) – sea surface temperature in Niño area 3.4 (SST3.4)" proves that even when the cross correlation is low, the time series' components can be closely related to each other. A full time and frequency domain description of this bivariate time series is given. The AMO–SST3.4 time series is shown to form a closed-feedback loop system with a 2-year memory. The coherence between AMO and SST3.4 is statistically significant at intermediate frequencies where the coherent spectra amount up to 55 % of the total spectral densities. The gain factors are also described. Some recommendations are offered regarding time series analysis in climatology.
url http://www.earth-syst-dynam.net/6/389/2015/esd-6-389-2015.pdf
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