Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background
Published version. Source at http://dx.doi.org/10.5194/esd-7-281-2016 In order to have a scaling description of the climate system that is not inherently non-stationary, the rapid shifts between stadials and interstadials during the last glaciation (the Dansgaard-Oeschger events) cannot be included...
Published in: | Earth System Dynamics |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
European Geosciences Union
2016
|
Subjects: | |
Online Access: | https://hdl.handle.net/10037/10362 https://doi.org/10.5194/esd-7-281-2016 |
id |
ftunivtroemsoe:oai:munin.uit.no:10037/10362 |
---|---|
record_format |
openpolar |
spelling |
ftunivtroemsoe:oai:munin.uit.no:10037/10362 2023-05-15T16:00:02+02:00 Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background Rypdal, Kristoffer Rypdal, Martin Wibe 2016-03-31 https://hdl.handle.net/10037/10362 https://doi.org/10.5194/esd-7-281-2016 eng eng European Geosciences Union Earth System Dynamics info:eu-repo/grantAgreement/RCN/KLIMAFORSK/229754/Norway/Long-range memory in Earths climate response and its implications for future global warming// Rypdal, M. and Rypdal, K.: Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background, Earth Syst. Dynam., 7, 281-293, doi:10.5194/esd-7-281-2016, 2016. FRIDAID 1350401 doi:10.5194/esd-7-281-2016 2190-4979 2190-4987 https://hdl.handle.net/10037/10362 openAccess VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 Journal article Tidsskriftartikkel Peer reviewed 2016 ftunivtroemsoe https://doi.org/10.5194/esd-7-281-2016 2021-06-25T17:55:03Z Published version. Source at http://dx.doi.org/10.5194/esd-7-281-2016 In order to have a scaling description of the climate system that is not inherently non-stationary, the rapid shifts between stadials and interstadials during the last glaciation (the Dansgaard-Oeschger events) cannot be included in the scaling law. The same is true for the shifts between the glacial and interglacial states in the Quaternary climate. When these events are omitted from a scaling analysis the climate noise is consistent with a 1=f law on timescales from months to 105 years. If the shift events are included, the effect is a break in the scaling with an apparent 1=f law, with > 1, for the low frequencies. No evidence of multifractal intermittency has been found in any of the temperature records investigated, and the events are not a natural consequence of multifractal scaling. Article in Journal/Newspaper Dansgaard-Oeschger events University of Tromsø: Munin Open Research Archive Earth System Dynamics 7 1 281 293 |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 |
spellingShingle |
VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 Rypdal, Kristoffer Rypdal, Martin Wibe Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
topic_facet |
VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 |
description |
Published version. Source at http://dx.doi.org/10.5194/esd-7-281-2016 In order to have a scaling description of the climate system that is not inherently non-stationary, the rapid shifts between stadials and interstadials during the last glaciation (the Dansgaard-Oeschger events) cannot be included in the scaling law. The same is true for the shifts between the glacial and interglacial states in the Quaternary climate. When these events are omitted from a scaling analysis the climate noise is consistent with a 1=f law on timescales from months to 105 years. If the shift events are included, the effect is a break in the scaling with an apparent 1=f law, with > 1, for the low frequencies. No evidence of multifractal intermittency has been found in any of the temperature records investigated, and the events are not a natural consequence of multifractal scaling. |
format |
Article in Journal/Newspaper |
author |
Rypdal, Kristoffer Rypdal, Martin Wibe |
author_facet |
Rypdal, Kristoffer Rypdal, Martin Wibe |
author_sort |
Rypdal, Kristoffer |
title |
Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
title_short |
Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
title_full |
Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
title_fullStr |
Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
title_full_unstemmed |
Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background |
title_sort |
late quaternary temperature variability described as abrupt transitions on a 1/f noise background |
publisher |
European Geosciences Union |
publishDate |
2016 |
url |
https://hdl.handle.net/10037/10362 https://doi.org/10.5194/esd-7-281-2016 |
genre |
Dansgaard-Oeschger events |
genre_facet |
Dansgaard-Oeschger events |
op_relation |
Earth System Dynamics info:eu-repo/grantAgreement/RCN/KLIMAFORSK/229754/Norway/Long-range memory in Earths climate response and its implications for future global warming// Rypdal, M. and Rypdal, K.: Late Quaternary temperature variability described as abrupt transitions on a 1/f noise background, Earth Syst. Dynam., 7, 281-293, doi:10.5194/esd-7-281-2016, 2016. FRIDAID 1350401 doi:10.5194/esd-7-281-2016 2190-4979 2190-4987 https://hdl.handle.net/10037/10362 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.5194/esd-7-281-2016 |
container_title |
Earth System Dynamics |
container_volume |
7 |
container_issue |
1 |
container_start_page |
281 |
op_container_end_page |
293 |
_version_ |
1766395905814036480 |