On the elimination of Bias Averaging-Errors in proxy records

Knowledge of and insight into past environmental conditions can be obtained by processing and analyzing proxies. The proxies need to be processed as precisely and accurately as possible, otherwise the conclusion of the analysis will be biased. A calibration method which reduces bias errors in the pr...

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Published in:Mathematical Geosciences
Main Authors: Beelaerts, Veerle, De Ridder, Fjo, Schmitz, Nele, Bauwens, Maite, Dehairs, Frank, Schoukens, Johan, Pintelon, Rik
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
Online Access:https://doi.org/10.1007/s11004-008-9193-1
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spelling ftopenagrar:oai:www.openagrar.de:openagrar_mods_00025227 2023-05-15T14:03:51+02:00 On the elimination of Bias Averaging-Errors in proxy records Beelaerts, Veerle De Ridder, Fjo Schmitz, Nele Bauwens, Maite Dehairs, Frank Schoukens, Johan Pintelon, Rik 2009 https://doi.org/10.1007/s11004-008-9193-1 https://www.openagrar.de/receive/openagrar_mods_00025227 eng eng Mathematical geosciences : the official journal of the International Association for Mathematical Geosciences -- Math. Geosci. -- 1874-8961 -- 2414226-8 https://doi.org/10.1007/s11004-008-9193-1 https://www.openagrar.de/receive/openagrar_mods_00025227 only signed in user all rights reserved info:eu-repo/semantics/restrictedAccess Text ddc:580 averaging -- signal processing -- calibration -- environmental proxies article Text 2009 ftopenagrar https://doi.org/10.1007/s11004-008-9193-1 2023-03-06T00:13:00Z Knowledge of and insight into past environmental conditions can be obtained by processing and analyzing proxies. The proxies need to be processed as precisely and accurately as possible, otherwise the conclusion of the analysis will be biased. A calibration method which reduces bias errors in the proxy measurements due to averaging is presented. Sampling with nonzero sample sizes causes an averaging of the true proxy signal over the volume of the sample. The method is applied on a linear synthetic record which results in an optimal correction for frequency components ranging from the dc-frequency (DC) to one half of the sample frequency (fs/2). Next, the method is tested on non-linear synthetic data where the signal is reconstructed reasonably well. Finally, the method is applied to a real vessel density record of R.mucronata from Makongeni, Kenya, and to a real delta deuterium record of ice core EDC from dome C, Antarctica. The method discussed in this paper is a valuable tool for the calibration of proxy measurements; it can be applied as a correction for low resolution measurements and expanded to other types of samples and proxies. Working with small sample sizes (high resolution) amounts to working near the detection limit, where the signal-to-noise-ratio is low. This correction method provides an alternative in which low resolution measurements can be upgraded to minimize the loss of information due to larger sample sizes. Article in Journal/Newspaper Antarc* Antarctica ice core OpenAgrar (OA) Mathematical Geosciences 41 2 129 144
institution Open Polar
collection OpenAgrar (OA)
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language English
topic Text
ddc:580
averaging -- signal processing -- calibration -- environmental proxies
spellingShingle Text
ddc:580
averaging -- signal processing -- calibration -- environmental proxies
Beelaerts, Veerle
De Ridder, Fjo
Schmitz, Nele
Bauwens, Maite
Dehairs, Frank
Schoukens, Johan
Pintelon, Rik
On the elimination of Bias Averaging-Errors in proxy records
topic_facet Text
ddc:580
averaging -- signal processing -- calibration -- environmental proxies
description Knowledge of and insight into past environmental conditions can be obtained by processing and analyzing proxies. The proxies need to be processed as precisely and accurately as possible, otherwise the conclusion of the analysis will be biased. A calibration method which reduces bias errors in the proxy measurements due to averaging is presented. Sampling with nonzero sample sizes causes an averaging of the true proxy signal over the volume of the sample. The method is applied on a linear synthetic record which results in an optimal correction for frequency components ranging from the dc-frequency (DC) to one half of the sample frequency (fs/2). Next, the method is tested on non-linear synthetic data where the signal is reconstructed reasonably well. Finally, the method is applied to a real vessel density record of R.mucronata from Makongeni, Kenya, and to a real delta deuterium record of ice core EDC from dome C, Antarctica. The method discussed in this paper is a valuable tool for the calibration of proxy measurements; it can be applied as a correction for low resolution measurements and expanded to other types of samples and proxies. Working with small sample sizes (high resolution) amounts to working near the detection limit, where the signal-to-noise-ratio is low. This correction method provides an alternative in which low resolution measurements can be upgraded to minimize the loss of information due to larger sample sizes.
format Article in Journal/Newspaper
author Beelaerts, Veerle
De Ridder, Fjo
Schmitz, Nele
Bauwens, Maite
Dehairs, Frank
Schoukens, Johan
Pintelon, Rik
author_facet Beelaerts, Veerle
De Ridder, Fjo
Schmitz, Nele
Bauwens, Maite
Dehairs, Frank
Schoukens, Johan
Pintelon, Rik
author_sort Beelaerts, Veerle
title On the elimination of Bias Averaging-Errors in proxy records
title_short On the elimination of Bias Averaging-Errors in proxy records
title_full On the elimination of Bias Averaging-Errors in proxy records
title_fullStr On the elimination of Bias Averaging-Errors in proxy records
title_full_unstemmed On the elimination of Bias Averaging-Errors in proxy records
title_sort on the elimination of bias averaging-errors in proxy records
publishDate 2009
url https://doi.org/10.1007/s11004-008-9193-1
https://www.openagrar.de/receive/openagrar_mods_00025227
genre Antarc*
Antarctica
ice core
genre_facet Antarc*
Antarctica
ice core
op_relation Mathematical geosciences : the official journal of the International Association for Mathematical Geosciences -- Math. Geosci. -- 1874-8961 -- 2414226-8
https://doi.org/10.1007/s11004-008-9193-1
https://www.openagrar.de/receive/openagrar_mods_00025227
op_rights only signed in user
all rights reserved
info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1007/s11004-008-9193-1
container_title Mathematical Geosciences
container_volume 41
container_issue 2
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