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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2015-06-01
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Online Access: | http://www.earth-syst-dynam.net/6/389/2015/esd-6-389-2015.pdf |
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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 |
work_keys_str_mv |
AT vprivalsky onstudyingrelationsbetweentimeseriesinclimatology |
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