Nonlinear Processes in Geophysics ©European Geophysical Society 2002
Abstract. The method of recurrence plots is extended to the cross recurrence plots (CRP) which, among others, enables the study of synchronization or time differences in two time series. This is emphasized in a distorted main diagonal in the cross recurrence plot, the line of synchronization (LOS)....
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.371.814 2023-05-15T17:10:01+02:00 Nonlinear Processes in Geophysics ©European Geophysical Society 2002 N. Marwan M. Thiel N. R. Nowaczyk The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.814 http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.814 http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf text 2001 ftciteseerx 2016-01-08T01:20:45Z Abstract. The method of recurrence plots is extended to the cross recurrence plots (CRP) which, among others, enables the study of synchronization or time differences in two time series. This is emphasized in a distorted main diagonal in the cross recurrence plot, the line of synchronization (LOS). A non-parametrical fit of this LOS can be used to rescale the time axis of the two data series (whereby one of them is compressed or stretched) so that they are synchronized. An application of this method to geophysical sediment core data illustrates its suitability for real data. The rock magnetic data of two different sediment cores from the Makarov Basin can be adjusted to each other by using this method, so that they are comparable. 1 Text makarov basin Unknown Makarov Basin ENVELOPE(170.000,170.000,87.000,87.000) |
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Open Polar |
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ftciteseerx |
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English |
description |
Abstract. The method of recurrence plots is extended to the cross recurrence plots (CRP) which, among others, enables the study of synchronization or time differences in two time series. This is emphasized in a distorted main diagonal in the cross recurrence plot, the line of synchronization (LOS). A non-parametrical fit of this LOS can be used to rescale the time axis of the two data series (whereby one of them is compressed or stretched) so that they are synchronized. An application of this method to geophysical sediment core data illustrates its suitability for real data. The rock magnetic data of two different sediment cores from the Makarov Basin can be adjusted to each other by using this method, so that they are comparable. 1 |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
N. Marwan M. Thiel N. R. Nowaczyk |
spellingShingle |
N. Marwan M. Thiel N. R. Nowaczyk Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
author_facet |
N. Marwan M. Thiel N. R. Nowaczyk |
author_sort |
N. Marwan |
title |
Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
title_short |
Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
title_full |
Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
title_fullStr |
Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
title_full_unstemmed |
Nonlinear Processes in Geophysics ©European Geophysical Society 2002 |
title_sort |
nonlinear processes in geophysics ©european geophysical society 2002 |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.814 http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf |
long_lat |
ENVELOPE(170.000,170.000,87.000,87.000) |
geographic |
Makarov Basin |
geographic_facet |
Makarov Basin |
genre |
makarov basin |
genre_facet |
makarov basin |
op_source |
http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.814 http://hal.archives-ouvertes.fr/docs/00/30/21/23/PDF/npg-9-325-2002.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766066426874953728 |