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Simple climatic indices for the tropical Atlantic Ocean and some applications
Abstract
Two indices related to the sea surface temperature (SST) variability in the tropical Atlantic are proposed. One index describes the SST averaged over the whole basin (30°N to 20°S, 60°W to 15°E), and the other illustrates a meridional dipole between the northern and southern hemispheres. The computational method for obtaining these indices is intentionally kept simple, the objective being to reproduce the signature of the main results previously provided from more complicated statistical analyses. Monthly time series for both indices are produced from 1964 up to the present time. The whole basin index exhibits principally a sustained warming which has intensified since about 1975, and it has a significant periodicity close to that of the quasi‐biennial oscillation. The dipole index exhibits a decadal‐scale variation, and its building up seems to be related to other worldwide climatic changes, as for instance El Niño / Southern Oscillation extreme episodes, rainfall variabilities over the Brazilian Nordeste and African Sahel.
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“This is not surpring because it is observed in some studies (Rajagopalane et al., 1998, Servain, 1991) that the Atlantic dipole exhibits decadal time scales.”
From Sea surface temperature patterns in the Tropical Atlantic: Principal component analysis and nonlinear principal component analysis (2017) · cites this paper as Servain, 1991
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Items 201–282 of 282
A Quasi‐Biennial Oscillation in the equatorial Atlantic Ocean
Tseng, L., & Mechoso, C. (2001) · doi:10.1029/2000gl011206 · Cited by 9
Planetary equatorial trapped waves in the Atlantic Ocean from TOPEX/Poseidon altimetry.
França, C., Wainer, I., de Mesquita, A. R., & Goni, G. (2003) · Elsevier Oceanography Series · doi:10.1016/s0422-9894(03)80148-4 · Cited by 8
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BackgroundDjakouré, S., Amouin, J., Kouadio, K. Y., & Kacou, M. (2024) · Atmosphere · doi:10.20944/preprints202308.2172.v1 · Cited by 8
Dimoune, D. M., Birol, F., Hernández, F., Léger, F., & Araújo, M. (2023) · Ocean science · doi:10.5194/os-19-251-2023 · Cited by 19
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Lima, J. P., & Alves, J. B. (2009) · doi:10.1590/s0102-77862009000300006 · Cited by 8
PREVISÃO REGIONAL DA CHUVA PARA O ESTADO DO CEARÁ ATRAVÉS DO PROJETO "TEMPO DE CHUVA": 1964-1999
Xavier, A., Dias, M. A. F. D. S., Dias, P. L. D. S., & Xavier, T. D. M. B. S. (2000) · doi:10.21168/rbrh.v5n3.p69-82 · Cited by 8
Weakened interannual Tropical Atlantic variability in CMIP6 historical simulations
Verona, L. S., Silva, P., Wainer, I. E. K. C., & Khodri, M. (2023) · Climate Dynamics · doi:10.1007/s00382-023-06696-9 · Cited by 9
“It is represented by an interhemispheric dipole pattern characterized by crossequatorial SST anomaly gradient, whose nodal line is displaced slightly north of the equator (Servain 1991; Xie and Carton 2004; Chang et al. 2006; Doi et al. 2009; Cabos et al. 2019).”
BackgroundKodja, D. J. (2018) · doi:10.70675/8896ce28zbc8dz46a6za8a7ze10aa65d34df · Cited by 7
“Ces changements observés reflètent les variations de la circulation atmosphérique, dans la Zone de Convergence Intertropicale (ZCIT), en particulier de l’interaction entre le système TerreOcéan-Atmosphère (Ardoin-Bardin, 2004 ; Alexander et al., 2006 ; Mahé, 2006).”
BackgroundInfluentialInternal Variability of the Tropical Atlantic Ocean
Jochum, M., Murtugudde, R. G., Malanotte‐Rizzoli, P., & Busalacchi, A. J. (2011) · Geophysical monograph · doi:10.1029/147gm11 · Cited by 12
Spatial-temporal evolution of the low frequency climate variability in the tropical Atlantic
Ayina, L.-H., & Servain, J. (2003) · Elsevier oceanography series · doi:10.1016/s0422-9894(03)80159-9 · Cited by 9
Self-citationVitório, E. L., Silva, T., Vilela, I., Santos, E., & Veleda, D. (2025) · Dynamics of atmospheres and oceans (Print) · doi:10.1016/j.dynatmoce.2025.101596 · Cited by 6
Indicadores Climáticos e a Produtividade de Soja no Rio Grande do Sul
Arsego, D. A., Ferraz, S., Streck, N. A., Cardoso, A. D. O., & Zanon, A. (2019) · Revista Brasileira de Meteorologia · doi:10.1590/0102-77863340024 · Cited by 6
“…- Rogers, 1985); Padrão do Pacífico América Norte (PNA - Wallace e Gutzler, 1981); Oscilação Decadal do Pacífico (PDO - Mantua et al., 1997); Modo Meridional do Atlântico (AMM - Servain, 1991); Oscilação Ártica (AO - Thompson e Wallace, 1998) e Oscilação Antártica (AAO - Thompson e Wallace, 2000).”
Alves, J. B., Campos, J. N. B., & Nascimento, L. S. V. (2008) · doi:10.1590/s0102-77862008000100008 · Cited by 6
Coupled ocean-atmosphere inter-decadal modes in the tropics
Goswami, B., & Thomas, M. A. (2000) · doi:10.2151/jmsj1965.78.6_765 · Cited by 6
“The El Nino and Southern Oscillation (ENSO)like inter-decadal oscillation in the Pacific (Zhang et al. 1997; Kachi and Nitta 1997) and the Atlantic inter-hemispheric dipole mode (Moura and Shukla 1981; Servain 1991; Carton et al. 1996) are two important modes of climate variability in the tropics and sub-tropics ident…”
BackgroundClauzet, G., & Wainer, I. (1999) · doi:10.1590/s1413-77391999000100006 · Cited by 6
Kenfack, C. S., Mkankam, F. K., Alory, G., Penhoat, Y. D., Hounkonnou, M. N., Vondou, D. A., & Jr., B. G. N. (2017) · Terrestrial, Atmospheric and Oceanic Sciences · doi:10.3319/tao.2016.08.29.01 · Cited by 5
Arsego, D. A., Ferraz, S., Streck, N. A., Cardoso, A. D. O., Zanon, A., & Cera, J. (2020) · Revista Brasileira de Meteorologia · doi:10.1590/0102-7786351033 · Cited by 5
“…et al., 1999)); Oscilação Decadal do Pacífico (ODP - (Mantua et al., 1997)); Oscilação Quase Bienal (QBO - (Angell & Korshover, 1962)); Modo Meridional do Atlântico (AMM - (Servain, 1991)); Oscilação Ártica (AO - (Thompson & Wallace, 1998)) e Oscilação Antártica (OAA - (Thompson & Wallace, 2000)).”
Empirical forecasts of tropical Atlantic sea surface temperature anomalies
Elvira, A. R. D., OrtizBeviá, M. J., & Cabos, W. (2000) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.49712656711 · Cited by 3
Servain, J., Wainer, I. E. K. C., & Dessier, A. (1998) · Comptes Rendus de l Académie des Sciences - Series IIA - Earth and Planetary Science · doi:10.1016/s1251-8050(98)80011-6 · Cited by 5
Self-citationVianna, M. L., & Menezes, V. V. (2003) · Elsevier oceanography series · doi:10.1016/s0422-9894(03)80145-9 · Cited by 5
“Servain (1991) found that the tropical Atlantic SST interannual variability may be expressed as a sum of a QB and a 13 year mode.”
BackgroundInfluentialThe dependence of hydropower planning in relation to the influence of climate in Northeast Brazil
Santos, N. D. Q., Lima, K., & Spyrides, M. H. (2022) · PLoS ONE · doi:10.1371/journal.pone.0259951 · Cited by 4
Eremeev, V., Jukov, A. N., Piontkovski, S. A., & Sizov, A. A. (2009) · doi:10.1080/00207230902731920 · Cited by 4
“For each region, the normalized area average of SST anomalies were calculated (from January to March) and used to estimate the Sargasso-Tropical Index (STI) proposed by Servain (1991).”
BackgroundMethodda Silva, E. M., Alves, J. B., de Castro, M. D., Vieira, V. D. P. P. B., & Campos, J. N. B. (2007) · doi:10.1590/s0102-77862007000100009 · Cited by 4
“Essa tabela serviu ano de 1991 (Tabela 3) os resultados associados as variáveis de entrada da Tabela 1, após a aplicação das regras de inferência, apresentaram um nível de pertinência de µ (1,0) para a condição de N para as variáveis analisadas no/sobre o Oceano Tropical, as inferências mostraram um µ (0,67) para a co…”
BackgroundInfluentialBomventi, T. N., Wainer, I., & Taschetto, A. S. (2006) · doi:10.1590/s0102-261x2006000400005 · Cited by 4
Durand, B., Servain, J., Laurent, H., & Machado, L. (2005) · doi:10.1175/jcli3400.1 · Cited by 4
“The in-phase correlation study between the normalized monthly anomalies of the tropical Atlantic latent heat flux and the convective coverage over NEB during its rainy season (FMAM) shows a dipole signature straddling the ITCZ, quite different from the SST dipole (Servain 1991).”
BackgroundSelf-citationCABOSNARVAEZ, W., Álvarez-García, F., & OrtizBeviá, M. J. (2002) · Tellus A Dynamic Meteorology and Oceanography · doi:10.3402/tellusa.v54i4.12151 · Cited by 5
Present-Day Climate Variability in the Tropical Atlantic
Chiang, J. C. H. (2004) · Advances in global change research · doi:10.1007/978-1-4020-2944-8_17 · Cited by 1
Hounsou‐Gbo, A., Hall, N. M. J., Cardoso, L., Júnior, F. D. C. V., & Martins, E. S. P. R. (2024) · International Journal of Climatology · doi:10.1002/joc.8746 · Cited by 3
“Concomitant positive SSTAs in the North and negative SSTAs in the South are referred to as the “positive Atlantic dipole,” and the opposite SSTA pattern is called the “negative Atlantic dipole” (Servain 1991; Carton et al. 1996; Hounsou-Gbo et al. 2019).”
Zhang, K., Meng, W., Liu, H., & Wu, R. (2023) · Atmospheric Research · doi:10.1016/j.atmosres.2023.106968 · Cited by 4
Fluvial connectivity in the Brazilian semi-arid, Araripe sedimentary plateau
de Lima, G. G., de Barros, A. C. M., Corrêa, A. C. D. B., & Marçal, M. (2022) · Physis Terrae - Revista Ibero-Afro-Americana de Geografia Física e Ambiente · doi:10.21814/physisterrae.4098 · Cited by 3
“…linked to global scale phenomena such as El Niño/Southern Oscillation and Atlantic Dipole (Hanstenrath & Heller, 1977; Ropelewski & Halpert, 1987; Servain, 1991; Nobre & Shukla, 1996; Brahmanada Rao et al ., 1997; Souza & Nobre, 1998; Haylock et al ., 2006; Andreoli & Kayano, 2007; Polzin &…”
BackgroundCaracterísticas Climatológicas dos Sistemas Convectivos de Mesoescala no Nordeste do Brasil
Jacinto, L. V., Eloi, W. M., & Sakamoto, M. S. (2022) · Revista Brasileira de Meteorologia · doi:10.1590/0102-77863710062 · Cited by 3
Local climate impacts of dipole-like sea surface temperature oscillations in the Southern Hemisphere
Oh, J.-H., & Jung, Y.-H. (2020) · doi:10.2166/wcc.2020.113 · Cited by 3
Braga, C. C., Amanajás, J., Cerqueira, H. D. V., & Vitorino, M. I. (2014) · doi:10.22564/rbgf.v32i1.399 · Cited by 3
“The years corresponding to either positive or negative dipole events were chosen based on the index proposed by Servain (1991).”
MethodGensac, E. (2012) · theses.fr (ABES) · doi:10.70675/35ec8d25z73d7z406ezaad8zc2eaf3b3da9f · Cited by 1
“Les deux principales variations climatiques sur l’Atlantique tropical s’exercent sur des échelles décennales et multi décennales (Servain, 1991 ; Metha et Delwoth, 1995, 1998) : (1) La première est du même type qu’El Niño dans le Pacifique.”
Backgroundda Silva, A. D., de Lacerda, L. D., & de Morais, J. O. (2012) · doi:10.22564/rbgf.v30i3.183 · Cited by 3
“The combination of the ITCZ position with other phenomena, like the Atlantic dipole (SST anomalies in the 1990; Servain, 1991).”
BackgroundSoares, L. A. M., Parise, C. K., Machado, A. M. B., Carpenedo, C. B., Furtado, T. M. S., Barreto, H. N., de Lima, L. G., & Sousa, H. L. S. (2023) · Ocean and Coastal Research · doi:10.1590/2675-2824072.22057lams · Cited by 3
ICE CORE RECORDS | South America
Thompson, L., & Davis, M. (2007) · doi:10.1016/b978-0-444-53643-3.00325-3 · Cited by 3
Camargo, S., Zebiak, S., Dewitt, D., & Goddard, L. (2001) · doi:10.7916/d8fb58s1 · Cited by 3
“The Atlantic Dipole index was defined following Servain [15].”
MethodAnálise da variabilidade espaço-temporal da precipitação em Maceió-AL e de suas causas climáticas
Cavalcante, I. B. D. S., da Silva, D. F., & Brandão, J. C. C. B. (2023) · Pesquisas em Geociências · doi:10.22456/1807-9806.123971 · Cited by 2
“…as seguintes escalas: sazonal (0,25 anos) (Weickmann et al. , 1985), semestral (0,5 anos) (Nascimento et al. , 2017), interanual (1 ano) (Servain, 1991), ENOS (entre 1 e 2 anos) ENOS estendido (2 a 7 anos) (Da Silva, 2017; Da Silva et al. , 2020), Manchas Solares (11 anos) (Kerr, 1996;…”
Dia-Diop, A., Wade, M., Zebaze, S., Diop, A., Efon, E., Lenouo, A., & Diop, B. (2021) · Atmospheric and Climate Sciences · doi:10.21203/rs.3.rs-263090/v1 · Cited by 2
“However, the peri-Atlantic regions are also concerned since Enoa is also associated with the variability of sea surface temperatures and trade winds over the tropical Atlantic ([6] [7] [8]).”
BackgroundInfluência da variabilidade interdecadal do clima associada ao ENOS sobre o estado do Ceará
da Silva, D. F. (2014) · Revista Ibero-Americana de Ciências Ambientais · doi:10.6008/ess2179-6858.2013.002.0005 · Cited by 2
Investigation of the Interannual Variability of the Tropical Atlantic Ocean from Satellite Data
Arnault, S., & Mélice, J. L. (2012) · Marine Geodesy · doi:10.1080/01490419.2012.718212 · Cited by 1
“1999; Tseng and Mechoso 2001), and into decadal timescale of variability, with sea-surface temperature (SST) varying almost in opposition north and south of the equator (Moura and Shukla 1981; Servain 1991; Houghton and Tourre 1992; Mélice and Servain 2003).”
BackgroundSizov, A. A., & Chekhlan, A. E. (2010) · doi:10.3103/s1068373910070071 · Cited by 2
CLIVAR workshop on tropical Atlantic variability
Garzoli, S., & Servain, J. (2003) · doi:10.1029/2002gl016823 · Cited by 2
“It is characterized by a north-south interhemispheric gradient of SST anomalies, and its time scale ranges from interannual to decadal [Moura and Shukla, 1981; Servain, 1991].”
BackgroundSelf-citationRegional aerosol emission reductions alter tropical circulation
Jeon, J.-G., Allen, R. J., Yeh, S.-W., Park, C.-E., Wilcox, L. J., Samset, B., Ahmadi, S., Ekman, A. M. L., Elling, M. T., Fraser-Leach, L., et al. (2026) · Environmental Research: Climate · doi:10.1088/2752-5295/ae9c63 · Cited by 1
“Because the warming and ascent are centered off the equator, over the subtropical North Atlantic rather than along the equator, this response resembles a positive Atlantic Meridional Mode (AMM) (Servain 1991, Chiang and Vimont 2004).”
InfluentialNeto, A. V. N., de Souza, E. B., Vasconcellos, F. C., Ferreira, D. B. D. S., Franco, V. S., da Costa, C. P. W., Jesus, E. D. S., & Tedeschi, R. G. (2025) · International Journal of Climatology · doi:10.1002/joc.8936 · Cited by 1
“…have been reported for the central-eastern Amazon and NEB, where it is notably associated with anomalous ITCZ displacement (Hastenrath 1984; Servain 1991; Nobre and Shukla 1996; Enfield and Mayer 1997; de Souza et al. 2000; Fu et al. 2001; Wang 2004; Donohoe et al. 2013; Pezzi and…”
Bincy Chandran, P., & Arunkumar, R. (2024) · ISH Journal of Hydraulic Engineering · doi:10.1080/09715010.2024.2394802 · Cited by 1
“Indices based on oceanic/atmospheric circulation are used to understand the dynamic behaviour of many hydrometeor-ological parameters (Servain 1991; Mathew et al. 2023).”
Pereira, M. P. S., Couto, F., Schumacher, V., Silva, F. D. D. S., Gomes, H. B., da Silva, D. F., Gomes, H. B., Costa, R. L., Justino, F., & Herdies, D. (2024) · Atmosphere · doi:10.3390/atmos15060713 · Cited by 1
Relationships between climate signals and warm spells in cold season over Iran
Pourasghar, F., & Babaeian, I. (2023) · Arabian Journal of Geosciences · doi:10.1007/s12517-023-11642-4 · Cited by 1
“The climate signals which used for exploring the relations with warm spells are as follows: North Atlantic Oscillation (NAO) is defined as the normalised pressure difference between a station on the Azores and Iceland (Jones et al.”
BackgroundInfluentialCauses and processes of two opposite climatic years in the tropical Atlantic warm pools
Cintra, M. M., Lentini, C. A. D., Servain, J., Araújo, M., Silva, M., & MENDES, D. G. (2022) · Dynamics of Atmospheres and Oceans · doi:10.1016/j.dynatmoce.2022.101337
Self-citationPrevisão de Temperatura da Superfície do Mar (TSM) no Atlântico Tropical com uso de Redes Neurais
Castro, E. S., Alves, J. M. B., da Silva, E. M., Campos, J. N. B., & Alves, A. O. (2020) · Revista Brasileira de Meteorologia · doi:10.1590/0102-77863540075 · Cited by 2
“Dentre eles destacam-se o Modo Equatorial, também chamado de El Niño do Atlântico (Zebiak, 1993) e o Modo Meridional, também denominado Gradiente Meridional de TSM ou Dipolo meridional (Moura; Shukla, 1981; Servain, 1991).”
BackgroundDownscaling dinâmico de precipitação e veranicos no estado do Ceará
Alves, J. B., da Silva, E. M., & Rickes, C. P. (2017) · doi:10.24221/jeap.2.4.2017.1428.385-393 · Cited by 1
“Entre eles, destacamos os estudos de Moura & SHukla (1981), Hastenrath (1984), Nobre & Shukla (1996), Alves et al. (1997, 2005), Uvo (1989), Souza; Alves & Repelli (1998), Servain (1991), Lucena, Servain & Gomes Filho (2011) e Alves (2012).”
BackgroundHua, L., & Yu, Y. (2015) · 气象学报:英文版 · doi:10.1007/s13351-015-4115-x · Cited by 1
“469 There are some interannual variation modes in SST anomalies in the tropical Atlantic (Melice 470 and Servain, 2003; Servain, 1991), but previous studies have rarely addressed the temperature 471 asymmetry in this basin.”
BackgroundNóbrega, R. S., & Santiago, G. A. C. F. (2014) · doi:10.4215/rm.v13i1.869 · Cited by 1
“…NEB com ENOS, mas estudos observacionais e estatísticos realizadas por Hastenrath e Heller (1977) e simulações numéricas por Moura e Shukla (1981), Servain (1991), Nobre e Shukla (1996), evidenciaram um padrão de anomalias da TSM sobre o oceano Atlântico tropical, comumente chamado de padrão de…”
BackgroundSizov, A. A., & Chekhlan, A. E. (2010) · doi:10.1007/s11110-010-9070-6 · Cited by 1
Scale interactions in the tropical Atlanticvariability simulated with a coupled GCM
Narváez, W. C., García, J. F. A., & Bevia, M. J. O. (2003) · doi:10.4401/ag-3382 · Cited by 1
“Additionally, there is an important decadal variability, associated with a ‘dipole pattern’, that explains roughly a 12% of the variability of the climatology-subtracted Sea Surface Temperature (hereinafter SST) field (Servain, 1991).”
Jochum, M. (2002) · doi:10.1575/1912/2601 · Cited by 1
“The inter- hemispheric (or dipole) mode, affects the gradient of the SST between the northern and southern tropics (Servain (1991)) and therefore influences the position of the ITCZ.”
BackgroundThe Climatology of Land-Falling Tropical Cyclones in North Carolina
Xie, L., Pietrafesa, L., & Wu, K. (2002) · doi:10.1061/40605(258)35 · Cited by 1
Analysis of climate influence on agricultural production in semiarid cearense
Silva, G., & da Silva, D. F. (2016) · doi:10.5935/1984-2295.20160044 · Cited by 1
“…1999); - Escala temporal de 11 anos se refere ao ciclo de Manchas solares (Kerr, 1996; Echer, 2003, Molion, 2005) e também ao Dipólo do Atlântico (Servain, 1991; Clauzet e Wainer, 1999); - Escala temporal de 20,2 - 22 anos, associada à Oscilação Decadal do Pacífico (ODP) (Mantua et al., 1997).”
BackgroundInfluentialInfluence Interdecadal (PDO and AMO) in Levels of the São Francisco River
da Silva, D. F. (2013) · Revista Brasileira de Geografia Física · doi:10.5935/1984-2295.20130044 · Cited by 3
Propagation of the sea-surface temperature anomalies in the Tropical Atlantic
Kayano, M. T., & Andreoli, R. V. (2003) · Meteorology and Atmospheric Physics · doi:10.1007/s00703-002-0600-8 · Cited by 1
“The equatorial mode has more pronounced variability on the IA timescale (e.g., Zebiak, 1993), while the inter-hemispheric mode is more conspicuous on the DD timescale (e.g., Servain, 1991; Houghton and Tourre, 1992; Carton et al, 1996; Chang et al, 1997; Tourre et al, 1999).”
BackgroundHounsou‐Gbo, A., Hall, N., Vasconcelos, F., Ferreira, A., Teixeira, C. E. P., Araújo, M., & Martins, E. (2026) · Journal of Geophysical Research - Oceans · doi:10.1029/2025jc023901
da Silva, R. R., Moura, G. B. D. A., Lopes, P., Nascimento, C. R., & Giongo, P. R. (2025) · Agriculture · doi:10.3390/agriculture15202162
“Água Preta (1), Amaraji (3), Barra de Guabiraba (4), Barreiros (5), Bonito (8), Cabo de Santo Agostinho (10), Catende (14), Ch ã de Alegria (15), Cort ê s (18), Escada (19), Gameleira (21), Glória do Goitá (22), Igarassu (24), Ipojuca (25), Itapissuma (27), Joaquim Nabuco (31), Maraial (38), Moreno (39), Palmares (41)…”
Spectral characteristics and ENSO relationship of the Paraná river streamflow
Kane, R. P. (2022) · Mausam · doi:10.54302/mausam.v56i2.939
“…is in contradiction with the spectral analysis of the North and South Atlantic SST indices (Kane, 1998b), where for data for 1964-90 (obtained from Servain, 1991), North Atlantic SST (28° N - 5° N) showed a periodicity of 10.9 years and the South-Atlantic SST (5° N - 20° S) showed a periodicity…”
ResultInfluentialWeakened Interannual Variability in the Tropical Atlantic
Verona, L., Silva, P., Wainer, I., & Khodri, M. (2021) · doi:10.21203/rs.3.rs-1108528/v1
“It is represented by an interhemispheric dipole pat-94 tern characterized by cross-equatorial SST anomaly gradient, whose nodal line95 is displaced slightly north of the equator (Servain, 1991; Xie and Carton, 2004;96 Chang et al, 2006; Doi et al, 2009; Cabos et al, 2019).”
BackgroundAssis, É. A., Alves, J. B., Silva, E. M., Vasconcelos, F. D. C., Barbosa, A. C., dos Santos, A. C. S., & Sombra, S. S. (2019) · Revista Brasileira de Meteorologia · doi:10.1590/0102-7786334036
Ferreira, F. F., da Silva, V. D. P. R., da Silva, L. L., da Silva, E. M., Alves, J. M. B., Bandeira, M. M., & Becker, C. T. (2016) · Revista Brasileira de Meteorologia · doi:10.1590/0102-778631320160050
“…de estudos observacionais que relacionaram a ocorrência de anos secos ou chuvosos na RSANEB com a ocorrência de El Niño ou La Niña no Oceano Pacífico e o sinal do Dipolo no Oceano Atlântico (Hastenrath e Heller, 1977; Moura e Shukla, 1981; Servain, 1993; Nobre e Shukla, 1996; Nobre, 2001).”
BackgroundDipole index of the tropical Atlantic and precipitation regime in Cote de Voire
Bamba, I. (2007) · doi:10.3103/s1068373907120060
“Abstract—J. Servain, a French scientist [ 21 ], proposed a dipole index of a thermal state of waters in the tropical Atlantic.”
BackgroundAir-sea interaction in the tropical Atlantic
Deppenmeier, A. (2019) · doi:10.18174/496766
Carlin (2002) · doi:10.1175/1520-0442(2002)015
Mutai, C. (2000) · doi:10.1175/1520-0442(2000)013
Carretero (1998) · doi:10.1175/1520-0477(1998)079
Self-citationLatif, M. (1999) · doi:10.1175/1520-0442(1999)012
Quesada (2001) · doi:10.1175/1520-0442(2001)014
(2003) · doi:10.1175/1520-0442(2003)016
“…its projection into the tropical Atlantic (e.g., Enfield and Mayer 1997), the tropical Atlantic meridional SST gradient (e.g., Moura and Shukla 1981; Servain 1991; Chang et al. 1997; Xie 1999; Enfield et al. 1999), the equatorial Atlantic El Niño (e.g., Zebiak 1993; Carton and Huang 1994; Latif…”
BackgroundServain (2000) · doi:10.1002/1097-0088(200007)20:9
Self-citationMcHugh, M. (2004) · doi:10.1175/1520-0442(2004)017
Vauclair (2004) · doi:10.1175/1520-0485(2004)034
Metadata
- Authors
- Servain, J.
- Corresponding author
- Servain, Jacques
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 1991-08-15
- Volume
- 96
- Issue
- C8
- Pages
- 15137-15146
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W1988245413
- Cited by
- 345
- References
- 0
- Citations by year
- 2026: 3 · 2025: 6 · 2024: 9 · 2023: 13 · 2022: 13 · 2021: 6 · 2020: 11 · 2019: 9 · 2018: 15 · 2017: 9 · 2016: 12 · 2015: 9 · 2014: 8 · 2013: 10 · 2012: 10
- FWCI
- 4.63
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Geophysical Research Atmospheres (publishedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- tropical Atlantic, sea surface temperature variability, climate indices, meridional dipole, quasi-biennial oscillation, decadal variability, ENSO, ocean warming
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