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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Published in:Climate
Main Authors: Knut Lehre Seip, Hui Wang
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2022
Subjects:
AMO
NAO
Q
Online Access:https://doi.org/10.3390/cli10050063
https://doaj.org/article/2ac28be577ab4885bf7a1b871d360049
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spelling 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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