The North Atlantic Oscillations: 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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ftdoajarticles:oai:doaj.org/article:2ac28be577ab4885bf7a1b871d360049 2023-05-15T17:28:42+02:00 The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis Knut Lehre Seip Hui Wang 2022-05-01T00:00:00Z https://doi.org/10.3390/cli10050063 https://doaj.org/article/2ac28be577ab4885bf7a1b871d360049 EN eng MDPI AG https://www.mdpi.com/2225-1154/10/5/63 https://doaj.org/toc/2225-1154 doi:10.3390/cli10050063 2225-1154 https://doaj.org/article/2ac28be577ab4885bf7a1b871d360049 Climate, Vol 10, Iss 63, p 63 (2022) climate ocean oscillations AMOC AMO NAO Lead–lag relations Science Q article 2022 ftdoajarticles https://doi.org/10.3390/cli10050063 2022-12-31T02:19:10Z 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. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Climate 10 5 63 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
climate ocean oscillations AMOC AMO NAO Lead–lag relations Science Q |
spellingShingle |
climate ocean oscillations AMOC AMO NAO Lead–lag relations Science Q Knut Lehre Seip Hui Wang The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
topic_facet |
climate ocean oscillations AMOC AMO NAO Lead–lag relations Science Q |
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. |
format |
Article in Journal/Newspaper |
author |
Knut Lehre Seip Hui Wang |
author_facet |
Knut Lehre Seip Hui Wang |
author_sort |
Knut Lehre Seip |
title |
The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
title_short |
The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
title_full |
The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
title_fullStr |
The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
title_full_unstemmed |
The North Atlantic Oscillations: Lead–Lag Relations for the NAO, the AMO, and the AMOC—A High-Resolution Lead–lag Analysis |
title_sort |
north atlantic oscillations: lead–lag relations for the nao, the amo, and the amoc—a high-resolution lead–lag analysis |
publisher |
MDPI AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/cli10050063 https://doaj.org/article/2ac28be577ab4885bf7a1b871d360049 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
Climate, Vol 10, Iss 63, p 63 (2022) |
op_relation |
https://www.mdpi.com/2225-1154/10/5/63 https://doaj.org/toc/2225-1154 doi:10.3390/cli10050063 2225-1154 https://doaj.org/article/2ac28be577ab4885bf7a1b871d360049 |
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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1766121546777100288 |