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: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
AMO
NAO
Online Access:https://doi.org/10.3390/cli10050063
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spelling ftmdpi:oai:mdpi.com:/2225-1154/10/5/63/ 2023-08-20T04:08:13+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 agris 2022-05-05 application/pdf https://doi.org/10.3390/cli10050063 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/cli10050063 https://creativecommons.org/licenses/by/4.0/ Climate; Volume 10; Issue 5; Pages: 63 climate ocean oscillations AMOC AMO NAO Lead–lag relations Text 2022 ftmdpi https://doi.org/10.3390/cli10050063 2023-08-01T04:57:23Z 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. Text North Atlantic North Atlantic oscillation MDPI Open Access Publishing Climate 10 5 63
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic climate
ocean oscillations
AMOC
AMO
NAO
Lead–lag relations
spellingShingle climate
ocean oscillations
AMOC
AMO
NAO
Lead–lag relations
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/cli10050063
op_coverage agris
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Climate; Volume 10; Issue 5; Pages: 63
op_relation https://dx.doi.org/10.3390/cli10050063
op_rights https://creativecommons.org/licenses/by/4.0/
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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