A nonstationary ENSO-NAO relationship due to AMO modulation

Many previous studies have demonstrated a high uncertainty in the relationship between the El Niño-Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO). In the present work, decadal modulation by the Atlantic Multidecadal Oscillation (AMO) is investigated as a possible cause of the nonst...

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Published in:Journal of Climate
Main Authors: Zhang, Wenjun, Mei, Xuebin, Geng, Xin, Turner, Andrew G., Jin, Fei-Fei
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2019
Subjects:
Online Access:https://centaur.reading.ac.uk/77663/
https://centaur.reading.ac.uk/77663/1/Zhangetal2018_jclim_accepted.pdf
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spelling ftunivreading:oai:centaur.reading.ac.uk:77663 2024-06-23T07:54:58+00:00 A nonstationary ENSO-NAO relationship due to AMO modulation Zhang, Wenjun Mei, Xuebin Geng, Xin Turner, Andrew G. Jin, Fei-Fei 2019-01 text https://centaur.reading.ac.uk/77663/ https://centaur.reading.ac.uk/77663/1/Zhangetal2018_jclim_accepted.pdf en eng American Meteorological Society https://centaur.reading.ac.uk/77663/1/Zhangetal2018_jclim_accepted.pdf Zhang, W., Mei, X., Geng, X., Turner, A. G. <https://centaur.reading.ac.uk/view/creators/90000510.html> orcid:0000-0002-0642-6876 and Jin, F.-F. (2019) A nonstationary ENSO-NAO relationship due to AMO modulation. Journal of Climate, 32. pp. 33-43. ISSN 1520-0442 doi: https://doi.org/10.1175/JCLI-D-18-0365.1 <https://doi.org/10.1175/JCLI-D-18-0365.1> Article PeerReviewed 2019 ftunivreading https://doi.org/10.1175/JCLI-D-18-0365.1 2024-06-11T15:07:33Z Many previous studies have demonstrated a high uncertainty in the relationship between the El Niño-Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO). In the present work, decadal modulation by the Atlantic Multidecadal Oscillation (AMO) is investigated as a possible cause of the nonstationary ENSO-NAO relationship based on observed and reanalysis data. It is found that the negative ENSO-NAO correlation in late winter is significant only when ENSO and the AMO are in-phase (AMO+/El Niño and AMO-/La Niña). However, no significant ENSO-driven atmospheric anomalies can be observed over the North Atlantic when ENSO and the AMO are out-of-phase (AMO-/El Niño and AMO+/La Niña). Further analysis indicates that the sea surface temperature anomaly (SSTA) in the tropical North Atlantic (TNA) plays an essential role in this modulating effect. Due to broadly analogous TNA SSTA responses to both ENSO and the AMO during late winter, a warm SSTA in the TNA is evident when El Niño occurs during a positive AMO phase, resulting in a significantly weakened NAO, and vice versa when La Niña occur during a negative AMO phase. In contrast, neither the TNA SSTA nor the NAO show a prominent change under out-of-phase combinations of ENSO and AMO. The AMO modulation and associated effect of the TNA SSTA are shown to be well reproduced by historical simulations of the HadCM3 coupled model and further verified by forced experiments using an atmospheric circulation model. These offer hope that similar models will be able to make predictions for the NAO when appropriately initialized. Article in Journal/Newspaper North Atlantic North Atlantic oscillation CentAUR: Central Archive at the University of Reading Journal of Climate 32 1 33 43
institution Open Polar
collection CentAUR: Central Archive at the University of Reading
op_collection_id ftunivreading
language English
description Many previous studies have demonstrated a high uncertainty in the relationship between the El Niño-Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO). In the present work, decadal modulation by the Atlantic Multidecadal Oscillation (AMO) is investigated as a possible cause of the nonstationary ENSO-NAO relationship based on observed and reanalysis data. It is found that the negative ENSO-NAO correlation in late winter is significant only when ENSO and the AMO are in-phase (AMO+/El Niño and AMO-/La Niña). However, no significant ENSO-driven atmospheric anomalies can be observed over the North Atlantic when ENSO and the AMO are out-of-phase (AMO-/El Niño and AMO+/La Niña). Further analysis indicates that the sea surface temperature anomaly (SSTA) in the tropical North Atlantic (TNA) plays an essential role in this modulating effect. Due to broadly analogous TNA SSTA responses to both ENSO and the AMO during late winter, a warm SSTA in the TNA is evident when El Niño occurs during a positive AMO phase, resulting in a significantly weakened NAO, and vice versa when La Niña occur during a negative AMO phase. In contrast, neither the TNA SSTA nor the NAO show a prominent change under out-of-phase combinations of ENSO and AMO. The AMO modulation and associated effect of the TNA SSTA are shown to be well reproduced by historical simulations of the HadCM3 coupled model and further verified by forced experiments using an atmospheric circulation model. These offer hope that similar models will be able to make predictions for the NAO when appropriately initialized.
format Article in Journal/Newspaper
author Zhang, Wenjun
Mei, Xuebin
Geng, Xin
Turner, Andrew G.
Jin, Fei-Fei
spellingShingle Zhang, Wenjun
Mei, Xuebin
Geng, Xin
Turner, Andrew G.
Jin, Fei-Fei
A nonstationary ENSO-NAO relationship due to AMO modulation
author_facet Zhang, Wenjun
Mei, Xuebin
Geng, Xin
Turner, Andrew G.
Jin, Fei-Fei
author_sort Zhang, Wenjun
title A nonstationary ENSO-NAO relationship due to AMO modulation
title_short A nonstationary ENSO-NAO relationship due to AMO modulation
title_full A nonstationary ENSO-NAO relationship due to AMO modulation
title_fullStr A nonstationary ENSO-NAO relationship due to AMO modulation
title_full_unstemmed A nonstationary ENSO-NAO relationship due to AMO modulation
title_sort nonstationary enso-nao relationship due to amo modulation
publisher American Meteorological Society
publishDate 2019
url https://centaur.reading.ac.uk/77663/
https://centaur.reading.ac.uk/77663/1/Zhangetal2018_jclim_accepted.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://centaur.reading.ac.uk/77663/1/Zhangetal2018_jclim_accepted.pdf
Zhang, W., Mei, X., Geng, X., Turner, A. G. <https://centaur.reading.ac.uk/view/creators/90000510.html> orcid:0000-0002-0642-6876 and Jin, F.-F. (2019) A nonstationary ENSO-NAO relationship due to AMO modulation. Journal of Climate, 32. pp. 33-43. ISSN 1520-0442 doi: https://doi.org/10.1175/JCLI-D-18-0365.1 <https://doi.org/10.1175/JCLI-D-18-0365.1>
op_doi https://doi.org/10.1175/JCLI-D-18-0365.1
container_title Journal of Climate
container_volume 32
container_issue 1
container_start_page 33
op_container_end_page 43
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