The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis
Several studies examine cycle periods and the interactions between the three major climate modes over the North Atlantic, namely the Atlantic meridional overturning circulation (AMOC), the Atlantic multidecadal oscillation (AMO), and the North Atlantic oscillation (NAO). Here, we use a relatively no...
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Online Access: | https://hdl.handle.net/11250/3034439 https://doi.org/10.3390/cli10050063 |
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fthsosloakersoda:oai:oda.oslomet.no:11250/3034439 2023-05-15T17:29:01+02:00 The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC. A High-Resolution Lead–Lag Analysis Seip, Knut Lehre Wang, Hui 2022-10-20T09:41:24Z application/pdf https://hdl.handle.net/11250/3034439 https://doi.org/10.3390/cli10050063 eng eng MDPI Climate. 2022, 10 (5), . urn:issn:2225-1154 https://hdl.handle.net/11250/3034439 https://doi.org/10.3390/cli10050063 cristin:2063077 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY Climate 10 5 0 Ocean oscillations Climate Lead–lag relations Peer reviewed Journal article 2022 fthsosloakersoda https://doi.org/10.3390/cli10050063 2022-11-30T23:37:01Z Several studies examine cycle periods and the interactions between the three major climate modes over the North Atlantic, namely the Atlantic meridional overturning circulation (AMOC), the Atlantic multidecadal oscillation (AMO), and the North Atlantic oscillation (NAO). Here, we use a relatively novel high-resolution Lead–lag (LL) method to identify short time windows with persistent LL relations in the three series during the period from 1947 to 2020. We find that there are roughly 20-year time windows where LL relations change direction at both interannual, high-frequency and multidecadal, low-frequency timescales. However, with varying LL strength, the AMO leads AMOC for the full period at the interannual timescale. During the period from 1980 to 2000, we had the sequence NAO!AMO!AMOC!NAO at the interannual timescale. For the full period in the decadal time scale, we obtain NAO!AMO!AMOC. The Ekman variability closely follows the NAO variability. Both single time series and the LL relation between pairs of series show pseudo-oscillating patterns with cycle periods of about 20 years. We list possible mechanisms that contribute to the cyclic behavior, but no conclusive evidence has yet been found. publishedVersion Article in Journal/Newspaper North Atlantic North Atlantic oscillation OsloMet (Oslo Metropolitan University): ODA (Open Digital Archive) Climate 10 5 63 |
institution |
Open Polar |
collection |
OsloMet (Oslo Metropolitan University): ODA (Open Digital Archive) |
op_collection_id |
fthsosloakersoda |
language |
English |
topic |
Ocean oscillations Climate Lead–lag relations |
spellingShingle |
Ocean oscillations Climate Lead–lag relations Seip, Knut Lehre Wang, Hui The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
topic_facet |
Ocean oscillations Climate Lead–lag relations |
description |
Several studies examine cycle periods and the interactions between the three major climate modes over the North Atlantic, namely the Atlantic meridional overturning circulation (AMOC), the Atlantic multidecadal oscillation (AMO), and the North Atlantic oscillation (NAO). Here, we use a relatively novel high-resolution Lead–lag (LL) method to identify short time windows with persistent LL relations in the three series during the period from 1947 to 2020. We find that there are roughly 20-year time windows where LL relations change direction at both interannual, high-frequency and multidecadal, low-frequency timescales. However, with varying LL strength, the AMO leads AMOC for the full period at the interannual timescale. During the period from 1980 to 2000, we had the sequence NAO!AMO!AMOC!NAO at the interannual timescale. For the full period in the decadal time scale, we obtain NAO!AMO!AMOC. The Ekman variability closely follows the NAO variability. Both single time series and the LL relation between pairs of series show pseudo-oscillating patterns with cycle periods of about 20 years. We list possible mechanisms that contribute to the cyclic behavior, but no conclusive evidence has yet been found. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Seip, Knut Lehre Wang, Hui |
author_facet |
Seip, Knut Lehre Wang, Hui |
author_sort |
Seip, Knut Lehre |
title |
The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
title_short |
The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
title_full |
The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
title_fullStr |
The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
title_full_unstemmed |
The North atlanticoOscillations: Lead–lag Relations for the NAO, the AMO, and the AMOC: A high-resolution lead–lag analysis |
title_sort |
north atlanticooscillations: lead–lag relations for the nao, the amo, and the amoc: a high-resolution lead–lag analysis |
publisher |
MDPI |
publishDate |
2022 |
url |
https://hdl.handle.net/11250/3034439 https://doi.org/10.3390/cli10050063 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
Climate 10 5 0 |
op_relation |
Climate. 2022, 10 (5), . urn:issn:2225-1154 https://hdl.handle.net/11250/3034439 https://doi.org/10.3390/cli10050063 cristin:2063077 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3390/cli10050063 |
container_title |
Climate |
container_volume |
10 |
container_issue |
5 |
container_start_page |
63 |
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1766122322267209728 |