Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis

Continuous flow analysis (CFA) has become a popular measuring technique for obtaining high-resolution chemical ice core records due to an attractive combination of measuring speed and resolution. However, when analyzing the deeper sections of ice cores or cores from low-accumulation areas, there is...

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Published in:Journal of Geophysical Research
Main Authors: Rasmussen, S. O., Andersen, K. K., Johnsen, S. J., Bigler, M., McCormack, T.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2005
Subjects:
Online Access:https://boris.unibe.ch/158305/1/rasmussen05jgr.pdf
https://boris.unibe.ch/158305/
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spelling ftunivbern:oai:boris.unibe.ch:158305 2023-08-20T04:02:00+02:00 Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis Rasmussen, S. O. Andersen, K. K. Johnsen, S. J. Bigler, M. McCormack, T. 2005 application/pdf https://boris.unibe.ch/158305/1/rasmussen05jgr.pdf https://boris.unibe.ch/158305/ eng eng American Geophysical Union https://boris.unibe.ch/158305/ info:eu-repo/semantics/openAccess Rasmussen, S. O.; Andersen, K. K.; Johnsen, S. J.; Bigler, M.; McCormack, T. (2005). Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis. Journal of Geophysical Research: Atmospheres, 110(D17), pp. 1-7. American Geophysical Union 10.1029/2004JD005717 <http://dx.doi.org/10.1029/2004JD005717> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2005 ftunivbern https://doi.org/10.1029/2004JD005717 2023-07-31T22:08:01Z Continuous flow analysis (CFA) has become a popular measuring technique for obtaining high-resolution chemical ice core records due to an attractive combination of measuring speed and resolution. However, when analyzing the deeper sections of ice cores or cores from low-accumulation areas, there is still need for further improvement of the resolution. Here a method for resolution enhancement of CFA data is presented. It is demonstrated that it is possible to improve the resolution of CFA data by restoring some of the detail that was lost in the measuring process, thus improving the usefulness of the data for high-resolution studies such as annual layer counting. The presented method uses deconvolution techniques and is robust to the presence of noise in the measurements. If integrated into the data processing, it requires no additional data collection. The method is applied to selected ice core data sequences from Greenland and Antarctica, and the results demonstrate that the data quality can be significantly improved. Article in Journal/Newspaper Antarc* Antarctica Greenland ice core BORIS (Bern Open Repository and Information System, University of Bern) Greenland Journal of Geophysical Research 110 D17
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Rasmussen, S. O.
Andersen, K. K.
Johnsen, S. J.
Bigler, M.
McCormack, T.
Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
topic_facet 530 Physics
description Continuous flow analysis (CFA) has become a popular measuring technique for obtaining high-resolution chemical ice core records due to an attractive combination of measuring speed and resolution. However, when analyzing the deeper sections of ice cores or cores from low-accumulation areas, there is still need for further improvement of the resolution. Here a method for resolution enhancement of CFA data is presented. It is demonstrated that it is possible to improve the resolution of CFA data by restoring some of the detail that was lost in the measuring process, thus improving the usefulness of the data for high-resolution studies such as annual layer counting. The presented method uses deconvolution techniques and is robust to the presence of noise in the measurements. If integrated into the data processing, it requires no additional data collection. The method is applied to selected ice core data sequences from Greenland and Antarctica, and the results demonstrate that the data quality can be significantly improved.
format Article in Journal/Newspaper
author Rasmussen, S. O.
Andersen, K. K.
Johnsen, S. J.
Bigler, M.
McCormack, T.
author_facet Rasmussen, S. O.
Andersen, K. K.
Johnsen, S. J.
Bigler, M.
McCormack, T.
author_sort Rasmussen, S. O.
title Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
title_short Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
title_full Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
title_fullStr Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
title_full_unstemmed Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
title_sort deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis
publisher American Geophysical Union
publishDate 2005
url https://boris.unibe.ch/158305/1/rasmussen05jgr.pdf
https://boris.unibe.ch/158305/
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
ice core
genre_facet Antarc*
Antarctica
Greenland
ice core
op_source Rasmussen, S. O.; Andersen, K. K.; Johnsen, S. J.; Bigler, M.; McCormack, T. (2005). Deconvolution-based resolution enhancement of chemical ice core records obtained by continuous flow analysis. Journal of Geophysical Research: Atmospheres, 110(D17), pp. 1-7. American Geophysical Union 10.1029/2004JD005717 <http://dx.doi.org/10.1029/2004JD005717>
op_relation https://boris.unibe.ch/158305/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1029/2004JD005717
container_title Journal of Geophysical Research
container_volume 110
container_issue D17
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