Empirically derived climate predictability over the extratropical northern hemisphere
A novel application of a technique developed from chaos theory is used in describing seasonal to interannual climate predictability over the Northern Hemisphere (NH). The technique is based on an empirical forecast scheme - local approximation in a reconstructed phase space - for time-series data. D...
Published in: | Nonlinear Processes in Geophysics |
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Online Access: | https://doi.org/10.5194/npg-1-41-1994 https://npg.copernicus.org/articles/1/41/1994/ |
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ftcopernicus:oai:publications.copernicus.org:npg32826 2023-05-15T17:31:10+02:00 Empirically derived climate predictability over the extratropical northern hemisphere Elsner, J. B. Tsonis, A. A. 2018-01-15 application/pdf https://doi.org/10.5194/npg-1-41-1994 https://npg.copernicus.org/articles/1/41/1994/ eng eng doi:10.5194/npg-1-41-1994 https://npg.copernicus.org/articles/1/41/1994/ eISSN: 1607-7946 Text 2018 ftcopernicus https://doi.org/10.5194/npg-1-41-1994 2020-07-20T16:28:16Z A novel application of a technique developed from chaos theory is used in describing seasonal to interannual climate predictability over the Northern Hemisphere (NH). The technique is based on an empirical forecast scheme - local approximation in a reconstructed phase space - for time-series data. Data are monthly 500 hPa heights on a latitude-longitude grid covering the NH from 20° N to the equator. Predictability is estimated based on the linear correlation between actual and predicted heights averaged over a forecast range of one- to twelve.month lead. The method is capable of extracting the major climate signals on this time scale including ENSO and the North Atlantic Oscillation. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Nonlinear Processes in Geophysics 1 1 41 44 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
A novel application of a technique developed from chaos theory is used in describing seasonal to interannual climate predictability over the Northern Hemisphere (NH). The technique is based on an empirical forecast scheme - local approximation in a reconstructed phase space - for time-series data. Data are monthly 500 hPa heights on a latitude-longitude grid covering the NH from 20° N to the equator. Predictability is estimated based on the linear correlation between actual and predicted heights averaged over a forecast range of one- to twelve.month lead. The method is capable of extracting the major climate signals on this time scale including ENSO and the North Atlantic Oscillation. |
format |
Text |
author |
Elsner, J. B. Tsonis, A. A. |
spellingShingle |
Elsner, J. B. Tsonis, A. A. Empirically derived climate predictability over the extratropical northern hemisphere |
author_facet |
Elsner, J. B. Tsonis, A. A. |
author_sort |
Elsner, J. B. |
title |
Empirically derived climate predictability over the extratropical northern hemisphere |
title_short |
Empirically derived climate predictability over the extratropical northern hemisphere |
title_full |
Empirically derived climate predictability over the extratropical northern hemisphere |
title_fullStr |
Empirically derived climate predictability over the extratropical northern hemisphere |
title_full_unstemmed |
Empirically derived climate predictability over the extratropical northern hemisphere |
title_sort |
empirically derived climate predictability over the extratropical northern hemisphere |
publishDate |
2018 |
url |
https://doi.org/10.5194/npg-1-41-1994 https://npg.copernicus.org/articles/1/41/1994/ |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
eISSN: 1607-7946 |
op_relation |
doi:10.5194/npg-1-41-1994 https://npg.copernicus.org/articles/1/41/1994/ |
op_doi |
https://doi.org/10.5194/npg-1-41-1994 |
container_title |
Nonlinear Processes in Geophysics |
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1 |
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1 |
container_start_page |
41 |
op_container_end_page |
44 |
_version_ |
1766128509547184128 |