Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing
6 pages, 6 figures In this work we have performed a detailed analysis, using signal processing tools, to study time series of data (temperature proxy) extracted from the GRIP ice-core records and we relate it with the evolution of atmospheric CO2 within the last glacial period. Our method is based i...
Published in: | Physics Letters A |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2007
|
Subjects: | |
Online Access: | http://hdl.handle.net/10261/15544 https://doi.org/10.1016/j.physleta.2007.02.035 |
id |
ftcsic:oai:digital.csic.es:10261/15544 |
---|---|
record_format |
openpolar |
spelling |
ftcsic:oai:digital.csic.es:10261/15544 2024-02-11T10:04:47+01:00 Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing Solé, Jordi Turiel, Antonio Llebot, Josep Enric 2007-02-14 131118 bytes application/pdf http://hdl.handle.net/10261/15544 https://doi.org/10.1016/j.physleta.2007.02.035 en eng Elsevier https://doi.org/10.1016/j.physleta.2007.02.035 Physics Letters A 366(3): 184-189 (2007) 0375-9601 http://hdl.handle.net/10261/15544 doi:10.1016/j.physleta.2007.02.035 none D/O events Climatic cycles Signal processing artículo http://purl.org/coar/resource_type/c_6501 2007 ftcsic https://doi.org/10.1016/j.physleta.2007.02.035 2024-01-16T09:23:04Z 6 pages, 6 figures In this work we have performed a detailed analysis, using signal processing tools, to study time series of data (temperature proxy) extracted from the GRIP ice-core records and we relate it with the evolution of atmospheric CO2 within the last glacial period. Our method is based in considering the warm periods known as Dansgaard–Oeschger (D/O) events and posterior returns to the cold stage as a climatic cycle. After the warming phase, D/O events relax to the initial cold state in three different ways, what gives rise to three classes of cycles. Also, the Younger/Dryas–Bolling/Allerod (Y/D–B/A) cycle corresponds to one of the classes obtained. We have found that all cycles start with identical warming phases which seem completely unrelated to variations in CO2 concentration. We discuss on the consequences for global climatology of such steady pattern of cycles A.T. is supported by Ramón y Cajal contract from MoE. J.E.L. acknowledges partial financial support of contract REN2003-00185. We are grateful to two anonymous referees for helpful criticism and constructive comments Peer reviewed Article in Journal/Newspaper ice core Digital.CSIC (Spanish National Research Council) Moe ENVELOPE(-45.683,-45.683,-60.733,-60.733) Physics Letters A 366 3 184 189 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
D/O events Climatic cycles Signal processing |
spellingShingle |
D/O events Climatic cycles Signal processing Solé, Jordi Turiel, Antonio Llebot, Josep Enric Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
topic_facet |
D/O events Climatic cycles Signal processing |
description |
6 pages, 6 figures In this work we have performed a detailed analysis, using signal processing tools, to study time series of data (temperature proxy) extracted from the GRIP ice-core records and we relate it with the evolution of atmospheric CO2 within the last glacial period. Our method is based in considering the warm periods known as Dansgaard–Oeschger (D/O) events and posterior returns to the cold stage as a climatic cycle. After the warming phase, D/O events relax to the initial cold state in three different ways, what gives rise to three classes of cycles. Also, the Younger/Dryas–Bolling/Allerod (Y/D–B/A) cycle corresponds to one of the classes obtained. We have found that all cycles start with identical warming phases which seem completely unrelated to variations in CO2 concentration. We discuss on the consequences for global climatology of such steady pattern of cycles A.T. is supported by Ramón y Cajal contract from MoE. J.E.L. acknowledges partial financial support of contract REN2003-00185. We are grateful to two anonymous referees for helpful criticism and constructive comments Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Solé, Jordi Turiel, Antonio Llebot, Josep Enric |
author_facet |
Solé, Jordi Turiel, Antonio Llebot, Josep Enric |
author_sort |
Solé, Jordi |
title |
Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
title_short |
Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
title_full |
Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
title_fullStr |
Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
title_full_unstemmed |
Classification of Dansgaard-Oeschger climatic cycles by the application of similitude signal processing |
title_sort |
classification of dansgaard-oeschger climatic cycles by the application of similitude signal processing |
publisher |
Elsevier |
publishDate |
2007 |
url |
http://hdl.handle.net/10261/15544 https://doi.org/10.1016/j.physleta.2007.02.035 |
long_lat |
ENVELOPE(-45.683,-45.683,-60.733,-60.733) |
geographic |
Moe |
geographic_facet |
Moe |
genre |
ice core |
genre_facet |
ice core |
op_relation |
https://doi.org/10.1016/j.physleta.2007.02.035 Physics Letters A 366(3): 184-189 (2007) 0375-9601 http://hdl.handle.net/10261/15544 doi:10.1016/j.physleta.2007.02.035 |
op_rights |
none |
op_doi |
https://doi.org/10.1016/j.physleta.2007.02.035 |
container_title |
Physics Letters A |
container_volume |
366 |
container_issue |
3 |
container_start_page |
184 |
op_container_end_page |
189 |
_version_ |
1790601528945410048 |