Nonlinear time series models for the North Atlantic Oscillation

The North Atlantic Oscillation (NAO) is the dominant mode of climate variability over the North Atlantic basin and has a significant impact on seasonal climate and surface weather conditions. This is the result of complex and nonlinear interactions between many spatio-temporal scales. Here, the auth...

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Published in:Advances in Statistical Climatology, Meteorology and Oceanography
Main Authors: T. Önskog, C. L. E. Franzke, A. Hannachi
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/ascmo-6-141-2020
https://doaj.org/article/639fae3ebef24bad80995c81f64bb682
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spelling ftdoajarticles:oai:doaj.org/article:639fae3ebef24bad80995c81f64bb682 2023-05-15T17:28:05+02:00 Nonlinear time series models for the North Atlantic Oscillation T. Önskog C. L. E. Franzke A. Hannachi 2020-10-01T00:00:00Z https://doi.org/10.5194/ascmo-6-141-2020 https://doaj.org/article/639fae3ebef24bad80995c81f64bb682 EN eng Copernicus Publications https://ascmo.copernicus.org/articles/6/141/2020/ascmo-6-141-2020.pdf https://doaj.org/toc/2364-3579 https://doaj.org/toc/2364-3587 doi:10.5194/ascmo-6-141-2020 2364-3579 2364-3587 https://doaj.org/article/639fae3ebef24bad80995c81f64bb682 Advances in Statistical Climatology, Meteorology and Oceanography, Vol 6, Pp 141-157 (2020) Oceanography GC1-1581 Meteorology. Climatology QC851-999 Probabilities. Mathematical statistics QA273-280 article 2020 ftdoajarticles https://doi.org/10.5194/ascmo-6-141-2020 2022-12-31T03:14:10Z The North Atlantic Oscillation (NAO) is the dominant mode of climate variability over the North Atlantic basin and has a significant impact on seasonal climate and surface weather conditions. This is the result of complex and nonlinear interactions between many spatio-temporal scales. Here, the authors study a number of linear and nonlinear models for a station-based time series of the daily winter NAO index. It is found that nonlinear autoregressive models, including both short and long lags, perform excellently in reproducing the characteristic statistical properties of the NAO, such as skewness and fat tails of the distribution, and the different timescales of the two phases. As a spin-off of the modelling procedure, we can deduce that the interannual dependence of the NAO mostly affects the positive phase, and that timescales of 1 to 3 weeks are more dominant for the negative phase. Furthermore, the statistical properties of the model make it useful for the generation of realistic climate noise. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Advances in Statistical Climatology, Meteorology and Oceanography 6 2 141 157
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Oceanography
GC1-1581
Meteorology. Climatology
QC851-999
Probabilities. Mathematical statistics
QA273-280
spellingShingle Oceanography
GC1-1581
Meteorology. Climatology
QC851-999
Probabilities. Mathematical statistics
QA273-280
T. Önskog
C. L. E. Franzke
A. Hannachi
Nonlinear time series models for the North Atlantic Oscillation
topic_facet Oceanography
GC1-1581
Meteorology. Climatology
QC851-999
Probabilities. Mathematical statistics
QA273-280
description The North Atlantic Oscillation (NAO) is the dominant mode of climate variability over the North Atlantic basin and has a significant impact on seasonal climate and surface weather conditions. This is the result of complex and nonlinear interactions between many spatio-temporal scales. Here, the authors study a number of linear and nonlinear models for a station-based time series of the daily winter NAO index. It is found that nonlinear autoregressive models, including both short and long lags, perform excellently in reproducing the characteristic statistical properties of the NAO, such as skewness and fat tails of the distribution, and the different timescales of the two phases. As a spin-off of the modelling procedure, we can deduce that the interannual dependence of the NAO mostly affects the positive phase, and that timescales of 1 to 3 weeks are more dominant for the negative phase. Furthermore, the statistical properties of the model make it useful for the generation of realistic climate noise.
format Article in Journal/Newspaper
author T. Önskog
C. L. E. Franzke
A. Hannachi
author_facet T. Önskog
C. L. E. Franzke
A. Hannachi
author_sort T. Önskog
title Nonlinear time series models for the North Atlantic Oscillation
title_short Nonlinear time series models for the North Atlantic Oscillation
title_full Nonlinear time series models for the North Atlantic Oscillation
title_fullStr Nonlinear time series models for the North Atlantic Oscillation
title_full_unstemmed Nonlinear time series models for the North Atlantic Oscillation
title_sort nonlinear time series models for the north atlantic oscillation
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/ascmo-6-141-2020
https://doaj.org/article/639fae3ebef24bad80995c81f64bb682
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Advances in Statistical Climatology, Meteorology and Oceanography, Vol 6, Pp 141-157 (2020)
op_relation https://ascmo.copernicus.org/articles/6/141/2020/ascmo-6-141-2020.pdf
https://doaj.org/toc/2364-3579
https://doaj.org/toc/2364-3587
doi:10.5194/ascmo-6-141-2020
2364-3579
2364-3587
https://doaj.org/article/639fae3ebef24bad80995c81f64bb682
op_doi https://doi.org/10.5194/ascmo-6-141-2020
container_title Advances in Statistical Climatology, Meteorology and Oceanography
container_volume 6
container_issue 2
container_start_page 141
op_container_end_page 157
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