Climate spectrum estimation in the presence of timescale errors

We introduce an algorithm (called REDFITmc2) for spectrum estimation in the presence of timescale errors. It is based on the Lomb-Scargle periodogram for unevenly spaced time series, in combination with the Welch's Overlapped Segment Averaging procedure, bootstrap bias correction and persistenc...

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Published in:Nonlinear Processes in Geophysics
Main Authors: Mudelsee, M., Scholz, D., Röthlisberger, R., Fleitmann, Dominik, Mangini, A., Wolff, E.W.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://boris.unibe.ch/38577/1/npg-16-43-2009.pdf
https://boris.unibe.ch/38577/
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spelling ftunivbern:oai:boris.unibe.ch:38577 2023-08-20T04:07:12+02:00 Climate spectrum estimation in the presence of timescale errors Mudelsee, M. Scholz, D. Röthlisberger, R. Fleitmann, Dominik Mangini, A. Wolff, E.W. 2009 application/pdf https://boris.unibe.ch/38577/1/npg-16-43-2009.pdf https://boris.unibe.ch/38577/ eng eng Copernicus Publications https://boris.unibe.ch/38577/ info:eu-repo/semantics/openAccess Mudelsee, M.; Scholz, D.; Röthlisberger, R.; Fleitmann, Dominik; Mangini, A.; Wolff, E.W. (2009). Climate spectrum estimation in the presence of timescale errors. Nonlinear processes in geophysics, 16(1), pp. 43-56. Göttingen: Copernicus Publications 10.5194/npg-16-43-2009 <http://dx.doi.org/10.5194/npg-16-43-2009> 550 Earth sciences & geology info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2009 ftunivbern https://doi.org/10.5194/npg-16-43-2009 2023-07-31T21:00:31Z We introduce an algorithm (called REDFITmc2) for spectrum estimation in the presence of timescale errors. It is based on the Lomb-Scargle periodogram for unevenly spaced time series, in combination with the Welch's Overlapped Segment Averaging procedure, bootstrap bias correction and persistence estimation. The timescale errors are modelled parametrically and included in the simulations for determining (1) the upper levels of the spectrum of the red-noise AR(1) alternative and (2) the uncertainty of the frequency of a spectral peak. Application of REDFITmc2 to ice core and stalagmite records of palaeoclimate allowed a more realistic evaluation of spectral peaks than when ignoring this source of uncertainty. The results support qualitatively the intuition that stronger effects on the spectrum estimate (decreased detectability and increased frequency uncertainty) occur for higher frequencies. The surplus information brought by algorithm REDFITmc2 is that those effects are quantified. Regarding timescale construction, not only the fixpoints, dating errors and the functional form of the age-depth model play a role. Also the joint distribution of all time points (serial correlation, stratigraphic order) determines spectrum estimation. Article in Journal/Newspaper ice core BORIS (Bern Open Repository and Information System, University of Bern) Nonlinear Processes in Geophysics 16 1 43 56
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 550 Earth sciences & geology
spellingShingle 550 Earth sciences & geology
Mudelsee, M.
Scholz, D.
Röthlisberger, R.
Fleitmann, Dominik
Mangini, A.
Wolff, E.W.
Climate spectrum estimation in the presence of timescale errors
topic_facet 550 Earth sciences & geology
description We introduce an algorithm (called REDFITmc2) for spectrum estimation in the presence of timescale errors. It is based on the Lomb-Scargle periodogram for unevenly spaced time series, in combination with the Welch's Overlapped Segment Averaging procedure, bootstrap bias correction and persistence estimation. The timescale errors are modelled parametrically and included in the simulations for determining (1) the upper levels of the spectrum of the red-noise AR(1) alternative and (2) the uncertainty of the frequency of a spectral peak. Application of REDFITmc2 to ice core and stalagmite records of palaeoclimate allowed a more realistic evaluation of spectral peaks than when ignoring this source of uncertainty. The results support qualitatively the intuition that stronger effects on the spectrum estimate (decreased detectability and increased frequency uncertainty) occur for higher frequencies. The surplus information brought by algorithm REDFITmc2 is that those effects are quantified. Regarding timescale construction, not only the fixpoints, dating errors and the functional form of the age-depth model play a role. Also the joint distribution of all time points (serial correlation, stratigraphic order) determines spectrum estimation.
format Article in Journal/Newspaper
author Mudelsee, M.
Scholz, D.
Röthlisberger, R.
Fleitmann, Dominik
Mangini, A.
Wolff, E.W.
author_facet Mudelsee, M.
Scholz, D.
Röthlisberger, R.
Fleitmann, Dominik
Mangini, A.
Wolff, E.W.
author_sort Mudelsee, M.
title Climate spectrum estimation in the presence of timescale errors
title_short Climate spectrum estimation in the presence of timescale errors
title_full Climate spectrum estimation in the presence of timescale errors
title_fullStr Climate spectrum estimation in the presence of timescale errors
title_full_unstemmed Climate spectrum estimation in the presence of timescale errors
title_sort climate spectrum estimation in the presence of timescale errors
publisher Copernicus Publications
publishDate 2009
url https://boris.unibe.ch/38577/1/npg-16-43-2009.pdf
https://boris.unibe.ch/38577/
genre ice core
genre_facet ice core
op_source Mudelsee, M.; Scholz, D.; Röthlisberger, R.; Fleitmann, Dominik; Mangini, A.; Wolff, E.W. (2009). Climate spectrum estimation in the presence of timescale errors. Nonlinear processes in geophysics, 16(1), pp. 43-56. Göttingen: Copernicus Publications 10.5194/npg-16-43-2009 <http://dx.doi.org/10.5194/npg-16-43-2009>
op_relation https://boris.unibe.ch/38577/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/npg-16-43-2009
container_title Nonlinear Processes in Geophysics
container_volume 16
container_issue 1
container_start_page 43
op_container_end_page 56
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