Cross recurrence plot based synchronization of time series
International audience 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 synchroniz...
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ftccsdartic:oai:HAL:hal-00302123v1 2023-11-12T04:20:49+01:00 Cross recurrence plot based synchronization of time series Marwan, N. Thiel, M. Nowaczyk, N. R. Institute of Physics Czech Academy of Sciences Prague (CAS) GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ) 2002 https://hal.science/hal-00302123 https://hal.science/hal-00302123/document https://hal.science/hal-00302123/file/npg-9-325-2002.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00302123 https://hal.science/hal-00302123 https://hal.science/hal-00302123/document https://hal.science/hal-00302123/file/npg-9-325-2002.pdf info:eu-repo/semantics/OpenAccess ISSN: 1023-5809 EISSN: 1607-7946 Nonlinear Processes in Geophysics https://hal.science/hal-00302123 Nonlinear Processes in Geophysics, 2002, 9 (3/4), pp.325-331 [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2002 ftccsdartic 2023-10-21T23:12:38Z International audience 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. Article in Journal/Newspaper makarov basin Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Makarov Basin ENVELOPE(170.000,170.000,87.000,87.000) |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Marwan, N. Thiel, M. Nowaczyk, N. R. Cross recurrence plot based synchronization of time series |
topic_facet |
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience 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. |
author2 |
Institute of Physics Czech Academy of Sciences Prague (CAS) GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ) |
format |
Article in Journal/Newspaper |
author |
Marwan, N. Thiel, M. Nowaczyk, N. R. |
author_facet |
Marwan, N. Thiel, M. Nowaczyk, N. R. |
author_sort |
Marwan, N. |
title |
Cross recurrence plot based synchronization of time series |
title_short |
Cross recurrence plot based synchronization of time series |
title_full |
Cross recurrence plot based synchronization of time series |
title_fullStr |
Cross recurrence plot based synchronization of time series |
title_full_unstemmed |
Cross recurrence plot based synchronization of time series |
title_sort |
cross recurrence plot based synchronization of time series |
publisher |
HAL CCSD |
publishDate |
2002 |
url |
https://hal.science/hal-00302123 https://hal.science/hal-00302123/document https://hal.science/hal-00302123/file/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 |
ISSN: 1023-5809 EISSN: 1607-7946 Nonlinear Processes in Geophysics https://hal.science/hal-00302123 Nonlinear Processes in Geophysics, 2002, 9 (3/4), pp.325-331 |
op_relation |
hal-00302123 https://hal.science/hal-00302123 https://hal.science/hal-00302123/document https://hal.science/hal-00302123/file/npg-9-325-2002.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1782336568430690304 |