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...

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Bibliographic Details
Main Authors: J. B. Elsner, A. A. Tsonis
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 1994
Subjects:
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Online Access:https://doaj.org/article/7f53bdac2ac24759b3eae81fd14e716a
Description
Summary: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.