On smoothing potentially non-stationary climate time series

[1] A simple approach to the smoothing of a potentially non-stationary time series is presented which provides an optimal choice among three alternative, readily motivated and easily implemented boundary constraints. This method is applied to the smoothing of the instrumental Northern Hemisphere (NH...

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Bibliographic Details
Main Author: Michael E. Mann
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
climate time series
Geophys. Res. Lett
31
L07214
North Atlantic
North Atlantic oscillation
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.2076
http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.364.2076
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.364.2076 2023-05-15T17:30:19+02:00 On smoothing potentially non-stationary climate time series Michael E. Mann The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.2076 http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.2076 http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf climate time series Geophys. Res. Lett 31 L07214 text ftciteseerx 2016-01-08T00:58:10Z [1] A simple approach to the smoothing of a potentially non-stationary time series is presented which provides an optimal choice among three alternative, readily motivated and easily implemented boundary constraints. This method is applied to the smoothing of the instrumental Northern Hemisphere (NH) annual mean and coldseason North Atlantic Oscillation (NAO) time series, yielding an objective estimate of the smoothed decadalscale variations in these series including long-term Text North Atlantic North Atlantic oscillation Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic climate time series
Geophys. Res. Lett
31
L07214
spellingShingle climate time series
Geophys. Res. Lett
31
L07214
Michael E. Mann
On smoothing potentially non-stationary climate time series
topic_facet climate time series
Geophys. Res. Lett
31
L07214
description [1] A simple approach to the smoothing of a potentially non-stationary time series is presented which provides an optimal choice among three alternative, readily motivated and easily implemented boundary constraints. This method is applied to the smoothing of the instrumental Northern Hemisphere (NH) annual mean and coldseason North Atlantic Oscillation (NAO) time series, yielding an objective estimate of the smoothed decadalscale variations in these series including long-term
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Michael E. Mann
author_facet Michael E. Mann
author_sort Michael E. Mann
title On smoothing potentially non-stationary climate time series
title_short On smoothing potentially non-stationary climate time series
title_full On smoothing potentially non-stationary climate time series
title_fullStr On smoothing potentially non-stationary climate time series
title_full_unstemmed On smoothing potentially non-stationary climate time series
title_sort on smoothing potentially non-stationary climate time series
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.2076
http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.2076
http://www.meteo.psu.edu/holocene/public_html/shared/articles/MannGRL04.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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