ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction

Linear dimensionality reduction techniques, notably principal component analysis, are widely used in climate data analysis as a means to aid in the interpretation of datasets of high dimensionality. These linear methods may not be appropriate for the analysis of data arising from nonlinear processes...

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Main Authors: I. Ross, P. J. Valdes, S. Wiggins
Format: Article
Language:English
Published: Copernicus Publications 2008-04-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/15/339/2008/npg-15-339-2008.pdf
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spelling doaj-aeefa54f86fc4dd3972f39e29e1fc9712020-11-24T21:01:32ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462008-04-01152339363ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reductionI. RossP. J. ValdesS. WigginsLinear dimensionality reduction techniques, notably principal component analysis, are widely used in climate data analysis as a means to aid in the interpretation of datasets of high dimensionality. These linear methods may not be appropriate for the analysis of data arising from nonlinear processes occurring in the climate system. Numerous techniques for nonlinear dimensionality reduction have been developed recently that may provide a potentially useful tool for the identification of low-dimensional manifolds in climate data sets arising from nonlinear dynamics. Here, we apply Isomap, one such technique, to the study of El Niño/Southern Oscillation variability in tropical Pacific sea surface temperatures, comparing observational data with simulations from a number of current coupled atmosphere-ocean general circulation models. We use Isomap to examine El Niño variability in the different datasets and assess the suitability of the Isomap approach for climate data analysis. We conclude that, for the application presented here, analysis using Isomap does not provide additional information beyond that already provided by principal component analysis. http://www.nonlin-processes-geophys.net/15/339/2008/npg-15-339-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Ross
P. J. Valdes
S. Wiggins
spellingShingle I. Ross
P. J. Valdes
S. Wiggins
ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
Nonlinear Processes in Geophysics
author_facet I. Ross
P. J. Valdes
S. Wiggins
author_sort I. Ross
title ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
title_short ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
title_full ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
title_fullStr ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
title_full_unstemmed ENSO dynamics in current climate models: an investigation using nonlinear dimensionality reduction
title_sort enso dynamics in current climate models: an investigation using nonlinear dimensionality reduction
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2008-04-01
description Linear dimensionality reduction techniques, notably principal component analysis, are widely used in climate data analysis as a means to aid in the interpretation of datasets of high dimensionality. These linear methods may not be appropriate for the analysis of data arising from nonlinear processes occurring in the climate system. Numerous techniques for nonlinear dimensionality reduction have been developed recently that may provide a potentially useful tool for the identification of low-dimensional manifolds in climate data sets arising from nonlinear dynamics. Here, we apply Isomap, one such technique, to the study of El Niño/Southern Oscillation variability in tropical Pacific sea surface temperatures, comparing observational data with simulations from a number of current coupled atmosphere-ocean general circulation models. We use Isomap to examine El Niño variability in the different datasets and assess the suitability of the Isomap approach for climate data analysis. We conclude that, for the application presented here, analysis using Isomap does not provide additional information beyond that already provided by principal component analysis.
url http://www.nonlin-processes-geophys.net/15/339/2008/npg-15-339-2008.pdf
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