Causes and processes of two opposite climatic years in the tropical Atlantic warm pools

International audience A numerical investigation of the interannual Southwestern and Equatorial Atlantic warm pools (WPs) (SST>28 °C) was conducted for the 2000-2014 period, focusing on two major opposite events over the past 39 years (1982-2020): an intense warming event in 2010 (sizeable warm p...

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Published in:Dynamics of Atmospheres and Oceans
Main Authors: Cintra, Marcio M., Lentini, Carlos A. D., Servain, Jacques, Araujo, Moacyr, Silva, Marcus, Mendes, David
Other Authors: Universidade Federal do Rio Grande do Norte Natal (UFRN), Universidade Federal da Bahia (UFBA), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Fundação Cearense de Meteorologia e Recursos Hídricos (FUNCEME)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://insu.hal.science/insu-03846479
https://doi.org/10.1016/j.dynatmoce.2022.101337
id ftunivparis:oai:HAL:insu-03846479v1
record_format openpolar
institution Open Polar
collection Université de Paris: Portail HAL
op_collection_id ftunivparis
language English
topic Temperature budget
Ocean-atmosphere interannual variability
Atlantic climatic variability modes
Tropical Atlantic warm pools
[SDU]Sciences of the Universe [physics]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle Temperature budget
Ocean-atmosphere interannual variability
Atlantic climatic variability modes
Tropical Atlantic warm pools
[SDU]Sciences of the Universe [physics]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Cintra, Marcio M.
Lentini, Carlos A. D.
Servain, Jacques
Araujo, Moacyr
Silva, Marcus
Mendes, David
Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
topic_facet Temperature budget
Ocean-atmosphere interannual variability
Atlantic climatic variability modes
Tropical Atlantic warm pools
[SDU]Sciences of the Universe [physics]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience A numerical investigation of the interannual Southwestern and Equatorial Atlantic warm pools (WPs) (SST>28 °C) was conducted for the 2000-2014 period, focusing on two major opposite events over the past 39 years (1982-2020): an intense warming event in 2010 (sizeable warm pool) and a moderate-to-low event in 2012 (small warm pool). Some modes of climate variability (remote and local) were confronted with the WP area. Significant remote connections were found for the North Atlantic Oscillation (NAO) and the Atlantic Meridional Mode (AMM). Whereas, the Tropical Northern Atlantic (TNA) and Tropical Southern Atlantic (TSA) indices were locally related to anomalies over the WP area. On the months that preceded the 2010 WP event, an anomalous atmospheric circulation in the tropical North Atlantic basin occurred (extremely negative NAO and positive AMM), causing a major weakening of winds, shallower mixed layer, and higher SST. Consequently, the WP boundaries, which usually developed southward along the equator in the austral fall, were pushed northward as warm waters spread out into the north tropical basin. Locally, both basins (i.e., tropical north and south) were warmer than climatologically expected (positive TNA and TSA), leading to a significant increase in the WP area recorded in this period. On the other hand, during the months that preceded the 2012 WP, the trade winds were faster (positive NAO and positive AMM), leading to a condition close to the climatologically expected. The approximation of the center of the subtropical high in the southern ocean basin practically extinguished the portion of warm waters that usually spreads southwest along the basin. While the TNA was weakly positive, the TSA presented negative anomalies that ensured a significant reduction in the WP area in the southern basin during this time. Numerical results from the 2000-2014 run were contrasted with PIRATA buoys and satellite data to assess the model's performance. Investigations of the mixed layer ...
author2 Universidade Federal do Rio Grande do Norte Natal (UFRN)
Universidade Federal da Bahia (UFBA)
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
Fundação Cearense de Meteorologia e Recursos Hídricos (FUNCEME)
format Article in Journal/Newspaper
author Cintra, Marcio M.
Lentini, Carlos A. D.
Servain, Jacques
Araujo, Moacyr
Silva, Marcus
Mendes, David
author_facet Cintra, Marcio M.
Lentini, Carlos A. D.
Servain, Jacques
Araujo, Moacyr
Silva, Marcus
Mendes, David
author_sort Cintra, Marcio M.
title Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
title_short Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
title_full Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
title_fullStr Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
title_full_unstemmed Causes and processes of two opposite climatic years in the tropical Atlantic warm pools
title_sort causes and processes of two opposite climatic years in the tropical atlantic warm pools
publisher HAL CCSD
publishDate 2022
url https://insu.hal.science/insu-03846479
https://doi.org/10.1016/j.dynatmoce.2022.101337
genre North Atlantic
North Atlantic oscillation
Southern Ocean
genre_facet North Atlantic
North Atlantic oscillation
Southern Ocean
op_source ISSN: 0377-0265
Dynamics of Atmospheres and Oceans
https://insu.hal.science/insu-03846479
Dynamics of Atmospheres and Oceans, 2022, 100, ⟨10.1016/j.dynatmoce.2022.101337⟩
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insu-03846479
https://insu.hal.science/insu-03846479
BIBCODE: 2022DyAtO.10001337C
doi:10.1016/j.dynatmoce.2022.101337
IRD: fdi:010086435
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container_title Dynamics of Atmospheres and Oceans
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spelling ftunivparis:oai:HAL:insu-03846479v1 2024-05-19T07:45:02+00:00 Causes and processes of two opposite climatic years in the tropical Atlantic warm pools Cintra, Marcio M. Lentini, Carlos A. D. Servain, Jacques Araujo, Moacyr Silva, Marcus Mendes, David Universidade Federal do Rio Grande do Norte Natal (UFRN) Universidade Federal da Bahia (UFBA) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Fundação Cearense de Meteorologia e Recursos Hídricos (FUNCEME) 2022 https://insu.hal.science/insu-03846479 https://doi.org/10.1016/j.dynatmoce.2022.101337 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.dynatmoce.2022.101337 insu-03846479 https://insu.hal.science/insu-03846479 BIBCODE: 2022DyAtO.10001337C doi:10.1016/j.dynatmoce.2022.101337 IRD: fdi:010086435 WOS: 000879107400001 ISSN: 0377-0265 Dynamics of Atmospheres and Oceans https://insu.hal.science/insu-03846479 Dynamics of Atmospheres and Oceans, 2022, 100, ⟨10.1016/j.dynatmoce.2022.101337⟩ Temperature budget Ocean-atmosphere interannual variability Atlantic climatic variability modes Tropical Atlantic warm pools [SDU]Sciences of the Universe [physics] [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2022 ftunivparis https://doi.org/10.1016/j.dynatmoce.2022.101337 2024-04-30T02:56:18Z International audience A numerical investigation of the interannual Southwestern and Equatorial Atlantic warm pools (WPs) (SST>28 °C) was conducted for the 2000-2014 period, focusing on two major opposite events over the past 39 years (1982-2020): an intense warming event in 2010 (sizeable warm pool) and a moderate-to-low event in 2012 (small warm pool). Some modes of climate variability (remote and local) were confronted with the WP area. Significant remote connections were found for the North Atlantic Oscillation (NAO) and the Atlantic Meridional Mode (AMM). Whereas, the Tropical Northern Atlantic (TNA) and Tropical Southern Atlantic (TSA) indices were locally related to anomalies over the WP area. On the months that preceded the 2010 WP event, an anomalous atmospheric circulation in the tropical North Atlantic basin occurred (extremely negative NAO and positive AMM), causing a major weakening of winds, shallower mixed layer, and higher SST. Consequently, the WP boundaries, which usually developed southward along the equator in the austral fall, were pushed northward as warm waters spread out into the north tropical basin. Locally, both basins (i.e., tropical north and south) were warmer than climatologically expected (positive TNA and TSA), leading to a significant increase in the WP area recorded in this period. On the other hand, during the months that preceded the 2012 WP, the trade winds were faster (positive NAO and positive AMM), leading to a condition close to the climatologically expected. The approximation of the center of the subtropical high in the southern ocean basin practically extinguished the portion of warm waters that usually spreads southwest along the basin. While the TNA was weakly positive, the TSA presented negative anomalies that ensured a significant reduction in the WP area in the southern basin during this time. Numerical results from the 2000-2014 run were contrasted with PIRATA buoys and satellite data to assess the model's performance. Investigations of the mixed layer ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation Southern Ocean Université de Paris: Portail HAL Dynamics of Atmospheres and Oceans 100 101337