Comparing climate time series – Part 3: Discriminant analysis

In parts I and II of this paper series, rigorous tests for equality of stochastic processes were proposed. These tests provide objective criteria for deciding whether two processes differ, but they provide no information about the nature of those differences. This paper develops a systematic and opt...

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Published in:Advances in Statistical Climatology, Meteorology and Oceanography
Main Authors: DelSole, Timothy, Tippett, Michael K.
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/ascmo-8-97-2022
https://ascmo.copernicus.org/articles/8/97/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:ascmo98394 2023-05-15T17:34:15+02:00 Comparing climate time series – Part 3: Discriminant analysis DelSole, Timothy Tippett, Michael K. 2022-05-16 application/pdf https://doi.org/10.5194/ascmo-8-97-2022 https://ascmo.copernicus.org/articles/8/97/2022/ eng eng doi:10.5194/ascmo-8-97-2022 https://ascmo.copernicus.org/articles/8/97/2022/ eISSN: 2364-3587 Text 2022 ftcopernicus https://doi.org/10.5194/ascmo-8-97-2022 2022-05-23T16:22:33Z In parts I and II of this paper series, rigorous tests for equality of stochastic processes were proposed. These tests provide objective criteria for deciding whether two processes differ, but they provide no information about the nature of those differences. This paper develops a systematic and optimal approach to diagnosing differences between multivariate stochastic processes. Like the tests, the diagnostics are framed in terms of vector autoregressive (VAR) models, which can be viewed as a dynamical system forced by random noise. The tests depend on two statistics, one that measures dissimilarity in dynamical operators and another that measures dissimilarity in noise covariances. Under suitable assumptions, these statistics are independent and can be tested separately for significance. If a term is significant, then the linear combination of variables that maximizes that term is obtained. The resulting indices contain all relevant information about differences between data sets. These techniques are applied to diagnose how the variability of annual-mean North Atlantic sea surface temperature differs between climate models and observations. For most models, differences in both noise processes and dynamics are important. Over 40 % of the differences in noise statistics can be explained by one or two discriminant components, though these components can be model dependent. Maximizing dissimilarity in dynamical operators identifies situations in which some climate models predict large-scale anomalies with the wrong sign. Text North Atlantic Copernicus Publications: E-Journals Advances in Statistical Climatology, Meteorology and Oceanography 8 1 97 115
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description In parts I and II of this paper series, rigorous tests for equality of stochastic processes were proposed. These tests provide objective criteria for deciding whether two processes differ, but they provide no information about the nature of those differences. This paper develops a systematic and optimal approach to diagnosing differences between multivariate stochastic processes. Like the tests, the diagnostics are framed in terms of vector autoregressive (VAR) models, which can be viewed as a dynamical system forced by random noise. The tests depend on two statistics, one that measures dissimilarity in dynamical operators and another that measures dissimilarity in noise covariances. Under suitable assumptions, these statistics are independent and can be tested separately for significance. If a term is significant, then the linear combination of variables that maximizes that term is obtained. The resulting indices contain all relevant information about differences between data sets. These techniques are applied to diagnose how the variability of annual-mean North Atlantic sea surface temperature differs between climate models and observations. For most models, differences in both noise processes and dynamics are important. Over 40 % of the differences in noise statistics can be explained by one or two discriminant components, though these components can be model dependent. Maximizing dissimilarity in dynamical operators identifies situations in which some climate models predict large-scale anomalies with the wrong sign.
format Text
author DelSole, Timothy
Tippett, Michael K.
spellingShingle DelSole, Timothy
Tippett, Michael K.
Comparing climate time series – Part 3: Discriminant analysis
author_facet DelSole, Timothy
Tippett, Michael K.
author_sort DelSole, Timothy
title Comparing climate time series – Part 3: Discriminant analysis
title_short Comparing climate time series – Part 3: Discriminant analysis
title_full Comparing climate time series – Part 3: Discriminant analysis
title_fullStr Comparing climate time series – Part 3: Discriminant analysis
title_full_unstemmed Comparing climate time series – Part 3: Discriminant analysis
title_sort comparing climate time series – part 3: discriminant analysis
publishDate 2022
url https://doi.org/10.5194/ascmo-8-97-2022
https://ascmo.copernicus.org/articles/8/97/2022/
genre North Atlantic
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op_source eISSN: 2364-3587
op_relation doi:10.5194/ascmo-8-97-2022
https://ascmo.copernicus.org/articles/8/97/2022/
op_doi https://doi.org/10.5194/ascmo-8-97-2022
container_title Advances in Statistical Climatology, Meteorology and Oceanography
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