Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation

Abstract The North Atlantic Oscillation (NAO) is a dominant atmospheric variability in the Northern Hemisphere that has a substantial impact on weather and climate on various time scales. Here, we investigate the role of energy conversion terms day‐by‐day during the NAO life cycle. The relative timi...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Kim, Minju, Sung, Mi‐Kyung, Yoo, Changhyun
Other Authors: National Research Foundation of Korea
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.4659
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4659
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spelling crwiley:10.1002/qj.4659 2024-06-02T08:11:14+00:00 Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation Kim, Minju Sung, Mi‐Kyung Yoo, Changhyun National Research Foundation of Korea 2024 http://dx.doi.org/10.1002/qj.4659 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4659 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Quarterly Journal of the Royal Meteorological Society volume 150, issue 760, page 1566-1580 ISSN 0035-9009 1477-870X journal-article 2024 crwiley https://doi.org/10.1002/qj.4659 2024-05-06T07:02:14Z Abstract The North Atlantic Oscillation (NAO) is a dominant atmospheric variability in the Northern Hemisphere that has a substantial impact on weather and climate on various time scales. Here, we investigate the role of energy conversion terms day‐by‐day during the NAO life cycle. The relative timing and contribution of the energy conversion terms are quantified by projecting the terms onto the eddy total energy, eddy kinetic energy (EKE), and eddy available potential energy (EAPE) patterns associated with the NAO. The results show a remarkable phase dependence in the growth and maintenance mechanisms. For positive NAOs, the initial growth is driven by the barotropic interactions between the eddies propagating over North America. This suggests that a non‐local growth mechanism plays an important role in the initiation of positive NAOs. In contrast, it is the baroclinic processes that initiate negative NAOs. The conversion of the mean APE into the EAPE and then into the EKE, processes which include eddy heat fluxes and vertical motions, results in the relatively local growth of negative NAOs. During the mature phase, the largest source of energy is the conversion of the mean APE into EAPE. Part of this is converted to EKE, making a substantial contribution to the maintenance of the EKE. This process is particularly important for negative NAOs. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Quarterly Journal of the Royal Meteorological Society 150 760 1566 1580
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The North Atlantic Oscillation (NAO) is a dominant atmospheric variability in the Northern Hemisphere that has a substantial impact on weather and climate on various time scales. Here, we investigate the role of energy conversion terms day‐by‐day during the NAO life cycle. The relative timing and contribution of the energy conversion terms are quantified by projecting the terms onto the eddy total energy, eddy kinetic energy (EKE), and eddy available potential energy (EAPE) patterns associated with the NAO. The results show a remarkable phase dependence in the growth and maintenance mechanisms. For positive NAOs, the initial growth is driven by the barotropic interactions between the eddies propagating over North America. This suggests that a non‐local growth mechanism plays an important role in the initiation of positive NAOs. In contrast, it is the baroclinic processes that initiate negative NAOs. The conversion of the mean APE into the EAPE and then into the EKE, processes which include eddy heat fluxes and vertical motions, results in the relatively local growth of negative NAOs. During the mature phase, the largest source of energy is the conversion of the mean APE into EAPE. Part of this is converted to EKE, making a substantial contribution to the maintenance of the EKE. This process is particularly important for negative NAOs.
author2 National Research Foundation of Korea
format Article in Journal/Newspaper
author Kim, Minju
Sung, Mi‐Kyung
Yoo, Changhyun
spellingShingle Kim, Minju
Sung, Mi‐Kyung
Yoo, Changhyun
Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
author_facet Kim, Minju
Sung, Mi‐Kyung
Yoo, Changhyun
author_sort Kim, Minju
title Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
title_short Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
title_full Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
title_fullStr Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
title_full_unstemmed Phase dependence of growth mechanisms in the daily energetics of the North Atlantic Oscillation
title_sort phase dependence of growth mechanisms in the daily energetics of the north atlantic oscillation
publisher Wiley
publishDate 2024
url http://dx.doi.org/10.1002/qj.4659
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4659
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Quarterly Journal of the Royal Meteorological Society
volume 150, issue 760, page 1566-1580
ISSN 0035-9009 1477-870X
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1002/qj.4659
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 150
container_issue 760
container_start_page 1566
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