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...
Published in: | Dynamics of Atmospheres and Oceans |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2022
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Online Access: | https://insu.hal.science/insu-03846479 https://doi.org/10.1016/j.dynatmoce.2022.101337 |
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ftsorbonneuniv:oai:HAL:insu-03846479v1 |
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openpolar |
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Open Polar |
collection |
HAL Sorbonne Université |
op_collection_id |
ftsorbonneuniv |
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) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-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) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-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⟩ |
op_relation |
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 |
op_doi |
https://doi.org/10.1016/j.dynatmoce.2022.101337 |
container_title |
Dynamics of Atmospheres and Oceans |
container_volume |
100 |
container_start_page |
101337 |
_version_ |
1810463409504780288 |
spelling |
ftsorbonneuniv:oai:HAL:insu-03846479v1 2024-09-15T18:23:14+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) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-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) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-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 ftsorbonneuniv https://doi.org/10.1016/j.dynatmoce.2022.101337 2024-08-01T23:46:51Z 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 HAL Sorbonne Université Dynamics of Atmospheres and Oceans 100 101337 |