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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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Westra, S., Brown, C., Lall, U., Koch, I., & Sharma, A. (2009) · International Journal of Climatology · doi:10.1002/joc.1888 · Cited by 39
“This polar behaviour across the ITCZ also can be observed by applying PCA to the Atlantic SSTA field, which is used as the basis of a dipole index (Weare, 1977; Hastenrath, 1978; Servain, 1991).”
MethodTourre, Y. M., Jarlan, L., Lacaux, J., Rotela, C. H., & Lafaye, M. (2008) · Environmental Research Letters · doi:10.1088/1748-9326/3/4/044008 · Cited by 37
“…indices such as: ‘NINO3’ in the equatorial Pacific Ocean (150◦W–90◦W and 3◦S–3◦N, from OGP/NOAA), ‘ATL3’ in the equatorial Atlantic Ocean (20◦W-GMT and 3◦S–3◦N, following Servain 1991), and the PSA 500 hPa geopotential index as defined by Mo (2000), and re-analyzed by Robertson and Mechoso (2003).”
MethodMultidecadal see-saw of the impact of ENSO on Indian and West African summer monsoon rainfall
Srivastava, G., Chakraborty, A., & Nanjundiah, R. S. (2018) · Climate Dynamics · doi:10.1007/s00382-018-4535-2 · Cited by 53
Atlantic Warm Pool Variability in the CMIP5 Simulations
Liu, H., Wang, C., Lee, S., & Enfield, D. B. (2013) · Journal of Climate · doi:10.1175/jcli-d-12-00556.1 · Cited by 33
“The correlations of the AWP with the tropical Atlantic meridional gradient mode (AMM) (Servain 1991; Chang et al. 1997, Xie et al. 1999; Enfield et al. 1999; Xie and Carton 2004) and theAtlantic Ni~no (Zebiak 1993; Carton and Huang 1994; Latif and Gr€otzner 2000; Okumura and Xie 2006) are statistically significant but…”
MethodLazar, A., Murtugudde, R., & Busalacchi, A. (2001) · doi:10.1029/2000gl011418 · Cited by 39
Prediction of tropical Atlantic sea surface temperature
Chang, P., Ji, L., Li, H., Penland, C., & Matrosova, L. (1998) · Geophysical Research Letters · doi:10.1029/98gl00852 · Cited by 33
de Medeiros, F. J., de Oliveira, C. P., & Torres, R. R. (2020) · Climate Dynamics · doi:10.1007/s00382-020-05385-1 · Cited by 43
“Positive (negative) GRAD index denotes the northward (southward) SST gradient over the intertropical Atlantic basin (Servain 1991; De Souza et al.”
BackgroundPhysical Processes Associated with the Tropical Atlantic SST Meridional Gradient
Hu, Z., & Huang, B. (2006) · Journal of Climate · doi:10.1175/jcli3923.1 · Cited by 38
Hasanean, H. M. (2004) · International Journal of Climatology · doi:10.1002/joc.1042 · Cited by 42
“Nevertheless, the index formed by the SST anomaly difference between the tropical North Atlantic and tropical South Atlantic (Servain, 1991), sometimes referred to as a dipole index, has proved to be an invaluable indicator of the meridional gradient in SST anomaly that is correlated with strong…”
BackgroundInfluentialDecadal oxygen change in the eastern tropical North Atlantic.
Hahn, J., Brandt, P., Schmidtko, S., & Krahmann, G. (2017) · Ocean Science · doi:10.5194/os-13-551-2017 · Cited by 38
“Servain (1991) introduced the AZM as the equatorial sea surface temperature (SST) anomaly and defined the AMM as the anomalous inter-hemispheric SST gradient with negative AMM corresponding to a negative/positive SST anomaly in the Northern/Southern Hemisphere.”
Kayano, M., Capistrano, V. B., Andreoli, R. V., & de Souza, R. D. (2016) · International Journal of Climatology · doi:10.1002/joc.4610 · Cited by 37
The variability of the tropical Atlantic
Cabos, W., OrtizBeviá, M. J., & Oberhuber, J. M. (1998) · Journal of Geophysical Research Atmospheres · doi:10.1029/97jc03419 · Cited by 22
Enfield, D. B., & Mestas‐Nuñez, A. M. (2010) · Cambridge University Press eBooks · doi:10.1017/cbo9780511573125.004 · Cited by 32
“…Atlantic (0°–20°S) SSTA regions to correlate antisymmetrical across the ITCZ in what is sometimes referred to as the tropical Atlantic dipole (Weare 1 Servain 1991), and for such covariability to be strongly related to rainfall anomalies in North Africa and Northeast Brazil (e.g., Moura and…”
BackgroundENSO forced and local variability of North Tropical Atlantic SST: model simulations and biases
Yang, Y., Xie, S., Wu, L., Kosaka, Y., & Li, J. (2017) · Climate Dynamics · doi:10.1007/s00382-017-3679-9 · Cited by 40
“Another important issue concerning the NTAM is the linkage with the Southern Tropical Atlantic Mode (STAM), as part of the tropical meridional mode (Servain 1991).”
BackgroundLucena, D. B., Servain, J., & Filho, M. F. G. (2011) · Journal of Climate · doi:10.1175/2011jcli4194.1 · Cited by 33
Self-citationRelationship between ocean climatic variability and rain-fed agriculture in northeast Brazil
Alves, J. M. B., Servain, J., & Campos, J. (2009) · Climate Research · doi:10.3354/cr00786 · Cited by 36
Self-citationThe impact of the subtropical South Atlantic SST on South American precipitation
Taschetto, A., & Wainer, I. (2008) · doi:10.5194/angeo-26-3457-2008 · Cited by 35
“In fact, the role of the SSTs on the ITCZ variations has been already reported by several authors (Moura and Shukla, 1981; Nobre and Shukla, 1996; Servain, 1991; Chang et al., 2000).”
BackgroundCoupled ocean wind and sea surface temperature patterns off the western Iberian Peninsula
Sánchez, R., Relvas, P., & Delgado, M. (2007) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2006.11.003 · Cited by 34
Losada, T., Rodríguez‐Fonseca, B., Mechoso, C. R., & Ma, H. (2007) · Climate Dynamics · doi:10.1007/s00382-007-0261-x · Cited by 32
Seasonal changes in the mixed and barrier layers in the western Equatorial Atlantic
da Silva, A. C., Araújo, M., Medeiros, C., Silva, M., & Bourlès, B. (2005) · Ocean and Coastal Research · doi:10.1590/s1679-87592005000200001 · Cited by 47
“, 1997) and dipole (Servain, 1991; Huang and Shukla, 1997) modes of low-frequency variabilities observed in this oceanic region.”
BackgroundCamberlin, P., & Diop, M. (1999) · Theoretical and Applied Climatology · doi:10.1007/s007040050101 · Cited by 34
“Numerous studies have shown that sea-surface temperatures (SST), both on global and regional (Atlantic ocean) scales, play a major part in the interannual variability of West African rainfall (Lamb, 1978; Hastenrath, 1984; Lough, 1986; Folland et al., 1986; Wolter, 1989; Servain 1991; Janicot, 1992b; Ward, 1992; Fonta…”
BackgroundAerosol-Induced Large-Scale Variability in Precipitation over the Tropical Atlantic
Huang, J., Zhang, C., & Prospero, J. M. (2009) · Journal of Climate · doi:10.1175/2009jcli2531.1 · Cited by 34
“…and the tropical Atlantic meridional mode SST index (SST anomaly difference between 58 and 258N, 558 and 158W and between 08 and 208S, 308W and 108E) (Servain 1991; Wang 2002). b. Analysis domains We focus mainly on precipitation variability in the Atlantic marine ITCZ (AMI), which has a strong…”
BackgroundTrzaska, S., Robertson, A. W., Farrara, J. D., & Mechoso, C. R. (2007) · Journal of Climate · doi:10.1175/jcli4114.1 · Cited by 32
“1999; Mo and Häkkinen 2001), and longer interannual time scales have been associated with northern Atlantic (Servain 1991; Tourre et al. 1999; Rajagopalan et al. 1998; Mo and Häkkinen 2001).”
BackgroundInfluentialRugg, A., Foltz, G. R., & Perez, R. C. (2016) · Journal of Climate · doi:10.1175/jcli-d-15-0867.1 · Cited by 38
“This definition is similar to that used by Servain (1991) (SST averaged over 58–288N, 608W–158E minus 208S–58N, 608W–158E), although we place a slightly stronger emphasis on lower latitudes, which are likely to affect atmospheric circulation and rainfall most strongly.”
BackgroundMethodA self-sustaining climate mode in the tropical Atlantic, 1995-97: Observations and modelling
Handoh, I. C., & Bigg, G. R. (2000) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.49712656403 · Cited by 32
Some characteristics and precipitation effects of the El Niño of 1997–1998
Kane, R. P. (1999) · doi:10.1016/s1364-6826(99)00087-5 · Cited by 32
Kayano, M. T., Andreoli, R. V., Garcia, S. R., & Souza, R. A. F. D. (2018) · International Journal of Climatology · doi:10.1002/joc.5545 · Cited by 33
“Some authors used the TA basins north and south of the thermal equator, 5 N, as the TNA and TSA representative areas (Servain, 1991; Melice and Servain, 2003; Huang et al., 2005).”
BackgroundInfluentialNóbrega, R. S., & Santiago, G. (2016) · doi:10.4067/s0718-34022016000100002 · Cited by 31
“Outros pesquisadores também destacam a relação entre a precipitação e o Atlântico Tropical em estudos observacionais e estatísticos, como as realizadas por Hastenrath e Heller (1977), e também com simulações numéricas por Moura e Shukla (1981), Servain (1991), Nobre e Shukla (1996).”
BackgroundCase studies in interannual to decadal climate predictability
Hermanson, L., & Sutton, R. (2010) · Climate Dynamics · doi:10.1007/s00382-009-0672-y · Cited by 31
“There is evidence of decadal variability in the tropical Atlantic, which is believed to have important climate impacts (Moura and Shukla 1981; Servain 1991 ).”
BackgroundRelação entre a precipitação do leste do Nordeste do Brasil e a temperatura dos oceanos
Moura, G. B. D. A., de Aragão, J. O. R., de Melo, J. S. P., da Silva, A. P. N., Giongo, P. R., & Lacerda, F. F. (2009) · Revista Brasileira de Engenharia Agrícola e Ambiental · doi:10.1590/s1415-43662009000400014 · Cited by 27
“Anomalias positivas de TSM no Atlântico Tropical sul produzem precipitação sobre o leste do NEB, enquanto anomalias positivas de TSM no Pacífico inibem a chuva no Leste do NEB. 3.”
BackgroundInfluentialJarlan, L., Tourre, Y., Mougin, E., Philippon, N., & Mazzega, P. (2005) · doi:10.1029/2004gl021841 · Cited by 31
“The indices used, represent signatures of climate signals and SST variability in various part of the tropical oceans such as: ‘‘NINO3’’ in the equatorial Pacific ocean (150W–90W and 3S–3N, from OGP/NOAA), ‘‘ATL3’’ in the equatorial Atlantic ocean (20W–GMT and 3S–3N, following Servain [1991] ), and ‘‘IO1’’ in the equat…”
MethodKiefer, J., & Karamperidou, C. (2019) · Paleoceanography and Paleoclimatology · doi:10.1029/2018pa003423 · Cited by 30
“In addition, Atlantic SST anomalies have been linked to precipitation anomalies in northeastern SA (e.g., Hastenrath & Heller, 1977; Nobre & Shukla, 1996; Servain, 1991), where positive (negative) equatorial Atlantic SST anomalies are correlated to abundant (deficient) rainfall.”
BackgroundVizy, E. K., & Cook, K. H. (2015) · Climate Dynamics · doi:10.1007/s00382-015-2691-1 · Cited by 43
“Two El Niño-like phenomena in the South Atlantic, namely Atlantic Niños and Benguela Niños, have also been identified (Servain 1991; Ruiz-Barradas et al. 2000).”
BackgroundXie, L., Yan, T., & Pietrafesa, L. J. (2005) · Geophysical Research Letters · doi:10.1029/2004gl021702 · Cited by 26
“Our study indicates that this Atlantic SST dipole mode (DM) [Servain, 1991] could have played an important role in creating Florida’s 2004 hurricane havoc.”
BackgroundDessay, N., Laurent, H., Machado, L., Shimabukuro, Y., Batista, G. T., Diédhiou, A., & Ronchail, J. (2004) · doi:10.1080/0143116031000101594 · Cited by 30
“For the Atlantic Ocean the observed SST of the north (28‡N– 5‡N; 60‡W–Africa) and south (5‡N–20‡ S; America–Africa) basins are from the monthly standardized SST anomalies dataset (1964–1999) provided by Servain (1991).”
BackgroundHormann, V., Lumpkin, R., & Foltz, G. R. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jc007697 · Cited by 41
“[28] Similar to Servain et al. [1999], we examined the relation between these modes and interannual ITCZ position anomalies (here based on a zero-wind stress-curl criterion), finding a good correlation between the meridional mode and”
MethodMatsuyama, H., Marengo, J., Obregón, G., & Nobre, C. (2002) · International Journal of Climatology · doi:10.1002/joc.724 · Cited by 29
Ocean Response and Feedback to the SST Dipole in the Tropical Atlantic*
Joyce, T. M., Frankignoul, C., Yang, J., & Phillips, H. E. (2004) · Journal of Physical Oceanography · doi:10.1175/jpo2640.1 · Cited by 25
“2), which leads us to somewhat smaller spatial regions than used by Servain (1991).”
BackgroundMethodJury, M. R. (2004) · Water SA · doi:10.4314/wsa.v29i1.4938 · Cited by 25
“…waves play a significant role in the generation of SST anomalies and coherent atmospheric responses and impacts (Nicholson and Entekhabi, 1987; Servain, 1991; Zebiak, 1993; D’Abreton and Lindesay, 1993; Curtis and Hastenrath, 1995; Mehta and Delworth, 1995; * To whom all correspondence should…”
BackgroundInterannual variability of the early and late-rainy seasons in the Caribbean
Martinez, C. J., Kushnir, Y., Goddard, L., & Ting, M. (2020) · Climate Dynamics · doi:10.1007/s00382-020-05341-z · Cited by 37
“2a–d, f–i) in the equatorial Atlantic is similar to the Atlantic Meridional Mode (AMM) a non-ENSO coupled ocean/atmosphere variability in the Atlantic basin (Servain 1991), of which has been found to be forced by the NAO (Chiang and Vimont 2004).”
Methodde Souza, R. A. F., Andreoli, R. V., Kayano, M. T., & Carvalho, A. L. (2015) · Geospatial Health · doi:10.4081/gh.2015.314 · Cited by 27
“This mode has been claimed to be one of the main features of the decadal variability in the tropical Atlantic (e.g., Servain, 1991; Andreoli and Kayano, 2003).”
BackgroundXie, L., Pietrafesa, L., & Wu, K. (2002) · doi:10.1007/s00376-002-0007-y · Cited by 27
100 Years of Progress in Understanding the Dynamics of Coupled Atmosphere–Ocean Variability
Battisti, D. S., Vimont, D. J., & Kirtman, B. P. (2019) · Meteorological Monographs · doi:10.1175/amsmonographs-d-18-0025.1 · Cited by 41
“Observational studies that focused on SST alone tended to reproduce the ‘‘dipole’’ structure (Servain 1991) formed by the northern and southern tropical Atlantic SST anomalies on multidecadal time scales, but emphasized the lack of interhemispheric coherence between the two centers of action on…”
BackgroundThermodynamic Coupled Modes in the Tropical Atmosphere–Ocean: An Analytical Solution
Wang, F. (2009) · Journal of the Atmospheric Sciences · doi:10.1175/2009jas3262.1 · Cited by 27
“In the tropical Atlantic, for example, the interhemispheric sea surface temperature (SST) gradient and the cross-equatorial surface wind display significant coherence on interannual– decadal time scales (Servain 1991; Nobre and Shukla 1996; Chang et al. 1997), which is known as the Atlantic meridional mode, causing st…”
BackgroundLoua, R. T., Benchérif, H., Mbatha, N., Bègue, N., Hauchecorne, A., Bamba, Z., & Sivakumar, V. (2019) · Climate · doi:10.3390/cli7070093 · Cited by 27
“It was originally identified by Servain [67].”
Mean and Variability of the Tropical Atlantic Ocean in the CCSM4*
Muñoz, E., Weijer, W., Grodsky, S. A., Bates, S. C., & Wainer, I. E. K. C. (2012) · Journal of Climate · doi:10.1175/jcli-d-11-00294.1 · Cited by 27
“Another mode of variability is the so-called zonal mode or Atlantic Nin˜o and is predominant in the boreal summer (Servain 1991; Tokinaga and Xie 2011; Carton and Huang 1994; Zebiak 1993; Shannon et al. 1986).”
BackgroundIllig, S., & Dewitte, B. (2006) · Journal of Climate · doi:10.1175/jcli3922.1 · Cited by 24
“At interannual time scales, two main modes emerge from observational studies: the meridional or dipole mode (Weare 1977; Servain 1991; Nobre and Shukla 1996; Corresponding author address: Serena Illig, LEGOS, 14 av. E. Belin, 31400 Toulouse, France.”
BackgroundEscalas temporais da variabilidade pluviométrica na bacia hidrográfica do Rio Mundaú
da Silva, D. F., de Sousa, F. D. A. S., & Kayano, M. T. (2010) · doi:10.1590/s0102-77862010000300004 · Cited by 24
“O modo de dipolo envolve variações de TSM em ambos os hemisférios, em escalas de tempo sazonal, interanual e decenal (Servain, 1991).”
BackgroundRole of tropical atlantic SST variability as a modulator of El Niño teleconnections
Ham, Y.-G., Sung, M., An, S., Schubert, S. D., & Kug, J. (2013) · Asia-Pacific Journal of Atmospheric Sciences · doi:10.1007/s13143-014-0013-x · Cited by 24
“Also, the ENSO-independent NATL variability is also possibly linked to the dipole mode reported in Moura and Shukla (1981), Servain and Legler (1986), and Servain (1991).”
BackgroundAtlantic Warm-Pool Variability in the IPCC AR4 CGCM Simulations
Liu, H., Wang, C., Lee, S., & Enfield, D. B. (2012) · Journal of Climate · doi:10.1175/jcli-d-11-00376.1 · Cited by 20
“Hence, there is a spuriously strong interaction between the zonal and AMM mode.”
BackgroundInfluentialTanimoto, Y., & Xie, S. (2002) · Journal of the Meteorological Society of Japan Ser II · doi:10.2151/jmsj.80.1199 · Cited by 86
“Then, SST anomalies are averaged for boreal winter and filtered through a decadal band of 8–16 year, a frequency domain that contains large SST variance (Servain 1991; Mehta 1998; Rajagopalan et al. 1998; Tourre et al. 1999).”
BackgroundA Linear Stability Analysis of Coupled Tropical Atlantic Variability
Wang, F., & Chang, P. (2008) · Journal of Climate · doi:10.1175/2007jcli2035.1 · Cited by 24
“…a dipole pattern in precipitation and an anomalous interhemispheric SST gradient, is believed to be a coupled mode intrinsic to the tropical Atlantic (Servain 1991; Mehta and Delworth 1995; Nobre and Shukla 1996; Tourre et al. 1999; Servain et al. 2000; Sutton et al. 2000; Chang et al. 2000, 2001).”
BackgroundRen, X., Zhang, L., Cai, W., Li, X., Wang, C., Jin, Y., & Wu, L. (2022) · Environmental Research Letters · doi:10.1088/1748-9326/ac8f5b · Cited by 22
“…the difference between the area-averaged SSTA (with ENSO influence removed) in north equatorial Atlantic (NEA, 0.5◦ N–20.5◦ N, 84.5◦ W–16.5◦ E) and south equatorial Atlantic (SEA, 0.5◦ S–20.5◦ S, 84.5◦ W–16.5◦ E), which is widely adopted in previous studies (Servain 1991, Melice and Servain 2003).”
ResultInfluentialVasconcelos, F. D. C., Jones, C., & Gandú, A. W. (2018) · Revista Brasileira de Meteorologia · doi:10.1590/0102-7786333007 · Cited by 21
da Silva, D. F. (2017) · doi:10.1590/0102-77863220002 · Cited by 21
“Autores associam-a ao ciclo de manchas solares e ao Dipolo do Atlântico (Servain, 1991; Kerr, 1996; Clauzet e Wainer, 1999; Echer, 2003; Molion, 2005).”
BackgroundMenezes, H. E. A., de Brito, J. I. B., dos Santos, C. A. C., & da Silva, L. L. (2008) · doi:10.1590/s0102-77862008000200004 · Cited by 21
Modes of tropical Atlantic climate variability observed by PIRATA
Servain, J., Clauzet, G., & Wainer, I. C. (2003) · Geophysical Research Letters · doi:10.1029/2002gl015124 · Cited by 21
“intertropical convergence zone (ITCZ) [Moura and Shukla, 1981; Servain, 1991].”
BackgroundInfluentialSelf-citationSST Indexes in the Tropical South Atlantic for Forecasting Rainy Seasons in Northeast Brazil
Hounsou‐Gbo, A., Servain, J., Araújo, M., Caniaux, G., Bourlès, B., Fontenele, D. P., & Martins, E. S. P. R. (2019) · Atmosphere · doi:10.3390/atmos10060335 · Cited by 28
“of sea surface temperature (SST) in the tropical Atlantic, which is associated with the anomalous latitudinal displacement of the ITCZ [5,7,8,13] between February and May.”
BackgroundResultInfluentialSelf-citationOceanic Indices for Forecasting Seasonal Rainfall over the Northern Part of Brazilian Northeast
Hounsou‐Gbo, A., Servain, J., Araújo, M., Martins, E. S. P. R., Bourlès, B., & Caniaux, G. (2016) · American Journal of Climate Change · doi:10.4236/ajcc.2016.52022 · Cited by 25
“Such LHF and PWS patterns agree quite well with the positive impact of the meridional SST gradient on the rainfall variability in the NNEB [4] [5], which has already been widely discussed in the literature (cold SST in the North, warm SST in the South) and is fully illustrated in Figure 4 of Hounsou-Gbo et al.”
BackgroundSelf-citationThe tropical ocean global atmosphere programme
Anderson, D. (1995) · doi:10.1080/00107519508230334 · Cited by 20
Seasonal predictability of the tropical Atlantic variability: northern tropical Atlantic pattern
Fang, G., & Huang, B. (2018) · Climate Dynamics · doi:10.1007/s00382-018-4556-x · Cited by 19
“On the other hand, NTA is closely linked to the Atlantic meridional mode (Chiang and Vimont 2004) and/or the dipole mode (Servain 1991), which emphasize the anomalous fluctuation of the cross-equatorial SST gradient.”
BackgroundAssessing low frequency variations in solar and wind power and their climatic teleconnections
Bianchi, E., Guozden, T., & Kozulj, R. (2022) · Renewable Energy · doi:10.1016/j.renene.2022.03.080 · Cited by 18
Teixeira, C. E. P., & Machado, G. T. (2013) · Journal of Coastal Research · doi:10.2112/si65-350.1 · Cited by 18
A fifty-year climatic signal in three Holocene stalagmite records from Mato Grosso, Brazil
Soubiès, F., Seidel, A., Mangin, A., Genty, D., Ronchail, J., Plagnes, V., Hirooka, S., & Santos, R. V. (2005) · Quaternary International · doi:10.1016/j.quaint.2004.10.027 · Cited by 15
Kane, R. P., & Buriti, R. (1997) · Pure and Applied Geophysics · doi:10.1007/s000240050052 · Cited by 18
“The fifth plot is for the tropical Atlantic basin (data from SERVAIN, 1991).”
BackgroundThe South Atlantic sub-tropical dipole mode since the last deglaciation and changes in rainfall
Wainer, I., Prado, L., Khodri, M., & Otto-Bliesner, B. (2020) · Climate Dynamics · doi:10.1007/s00382-020-05468-z · Cited by 17
“For example, the studies of (Moura and Shukla 1981; Servain 1991; Wainer and Soares 1997; Hastenrath 2012) among others, all related changes in Tropical SST with the migration of the Intertropical Convergence Zone (ITCZ) and rainfall in Brazil, particularly in its Northeast region (NEB).”
Black Carbon and West African Monsoon precipitation: observations and simulations
Huang, J., Adams, A., Wang, C., & Zhang, C. (2009) · Annales Geophysicae · doi:10.5194/angeo-27-4171-2009 · Cited by 17
“0 index (3◦ S–3◦ N, 20◦ W–0◦, Zebiak, 1993), and the TNA-TSA index (SST anomaly difference between 5◦–25◦ N, 55◦–15◦ W and 0◦–20◦ S, 30◦ W–10◦ E, Servain, 1991), were used in a multi-variable regression technique to remove their coherent signals in both aerosol and precipitation time series.”
Mora, G., & Martínez, J. (2005) · doi:10.1029/2005pa001132 · Cited by 17
Equatorial currents transport changes for extreme warm and cold events in the Atlantic Ocean
Góes, M., & Wainer, I. E. K. C. (2003) · Geophysical Research Letters · doi:10.1029/2002gl015707 · Cited by 19
“[2] With respect to sea surface temperature (SST), the tropical Atlantic ocean displays two dominant modes of interanual variability largely described in the literature [e.g. Servain, 1991; Wainer et al., 2002; Servain et al., 2002].”
BackgroundKane, R. P. (2001) · doi:10.1590/s0102-261x2001000200010 · Cited by 17
“Using the SST and wind component indices given by Hastenrath (1990), Rao et al. (1993), Servain (1991) and Servain and Lukas (1990) for the Atlantic region and the NE Brazil coast, Kane (1999) showed that for some El Niño events shown in Table 2, the droughts did not occur because the Atlantic…”
Method18 Environmental forcing and fisheries resources in Côte d'Ivoire and Ghana: Did something happen?
Cury, P. M., & Roy, C. (2002) · Large marine ecosystems · doi:10.1016/s1570-0461(02)80040-4 · Cited by 15
Interannual Climate Variations Over the Tropical Atlantic Ocean
Servain, J., & Merle, J. (1993) · Springer eBooks · doi:10.1007/978-3-642-76960-3_8 · Cited by 17
Self-citationCoupled Variability and Predictability in a Stochastic Climate Model of the Tropical Atlantic
Wang, F., & Chang, P. (2008) · Journal of Climate · doi:10.1175/2008jcli2283.1 · Cited by 19
“Rather, it displays two modes of variability: a decadal meridional sea surface temperature (SST) gradient mode coupled with cross-equatorial wind anomalies and an interannual zonal SST mode coupled with along-equatorial wind anomalies (e.g., Servain 1991; Tanimoto and Xie 1999).”
BackgroundAndreoli, R. V., & Kayano, M. T. (2003) · Meteorology and Atmospheric Physics · doi:10.1007/s00703-002-0568-4 · Cited by 17
El Niño and the Southern Oscillation: The Tropical Ice Core Record of ENSO
Thompson, L., Henderson, K., Mosley-Thompson, E., & Lin, P. (2000) · doi:10.1017/cbo9780511573125.010 · Cited by 16
Nnamchi, H. C., Dike, V. N., Akinsanola, A. A., & Okoro, U. K. (2021) · Atmospheric Research · doi:10.1016/j.atmosres.2021.105677 · Cited by 20
Alves, B., de Souza, F. D. A., & Silveira, C. D. S. (2013) · doi:10.21168/rbrh.v18n4.p19-34 · Cited by 15
Rao, V. B., Chapa, S. R., & Franchito, S. H. (1999) · Journal of the Meteorological Society of Japan Ser II · doi:10.2151/jmsj1965.77.1_63 · Cited by 16
Coral records of climate change: understanding past variability in the tropical ocean-atmosphere
Cole, J. (1996) · doi:10.1007/978-3-642-61113-1_16 · Cited by 15
Builes‐Jaramillo, A., Ramos, A. M. T., & Poveda, G. (2018) · Chaos An Interdisciplinary Journal of Nonlinear Science · doi:10.1063/1.5020502 · Cited by 23
Evangelista, H., Sifeddine, A., Corrège, T., Servain, J., Dassié, É. P., Logato, R., Cordeiro, R. C., Shen, C., Cornec, F. L., Nogueira, J. C. B., et al. (2018) · Geochemistry Geophysics Geosystems · doi:10.1002/2017gc007365 · Cited by 17
“…instance the meridional gradient in sea surface temperature (SST) linked to changes in trade winds (Covey & Hastenrath, 1978; Handoh et al., 2006; Servain, 1991; Zhang & Delworth, 2005) and the InterTropical Convergence Zone (ITCZ), a broad region of low atmospheric pressure, transporting water…”
BackgroundSelf-citationLucena, D. B., Filho, M. F. G., & Servain, J. (2011) · Revista Brasileira de Meteorologia · doi:10.1590/s0102-77862011000200013 · Cited by 15
“Por outro lado, os anos correspondentes aos anos com GRADM positivo ou negativo foram escolhidos com base no cálculo do índice proposto por Servain (1991), que consiste na diferença entre as médias da TSM na área delimitada na bacia norte do Atlântico por 60ºW-20ºW, 5ºN-28ºN, menos a área na bacia…”
BackgroundInfluentialSelf-citationIs the decadal variability in the tropical Atlantic a precursor to the NAO?
Wainer, I. E. K. C., Servain, J., & Clauzet, G. (2008) · Annales Geophysicae · doi:10.5194/angeo-26-4075-2008 · Cited by 11
“Nonetheless, the decadal signal is prominent be- tween the the years 1960–1990 (e.g. Servain, 1991).”
BackgroundInfluentialSelf-citationClimate variability modes due to ocean atmosphere interaction in the central Atlantic
Bojariu, R. (1997) · doi:10.3402/tellusa.v49i3.14675 · Cited by 13
On forecasting abnormal climatic events in the tropical Atlantic Ocean
Servain, J., & Arnault, S. (1995) · Annales Geophysicae · doi:10.1007/s00585-995-0995-x · Cited by 13
Self-citationArteaga, V. L., & Lima, C. (2020) · International Journal of Climatology · doi:10.1002/joc.6627 · Cited by 11
“The dipole index was originally proposed by Servain (1991), who defined the index based on SST anomalies in tropical regions of the Atlantic ocean.”
MethodAlves, J. M. B., Vasconcelos, F., Chaves, R. R., Silva, E. M., Servain, J., Costa, A., Sombra, S. S., Barbosa, A., & dos Santos, A. C. (2016) · Frontiers in Earth Science · doi:10.3389/feart.2016.00044 · Cited by 12
“This uncertainty is a result of the lack of quality of the coupled ocean-atmosphere models in representing the amplitude and frequency of ENSO events, and primarily in representing the Tropical Atlantic Sea Surface Temperature (SST) variability, once that their SST modes drive the annual rainfall anomalies in NNB (Ser…”
BackgroundSelf-citationThe relationships between tropical Atlantic sea level variability and major climate indices
Andrew, J. A. M., Leach, H., & Woodworth, P. L. (2006) · Ocean Dynamics · doi:10.1007/s10236-006-0068-z · Cited by 10
“Enfield and Mayer 1997, Fig. 5). Aside from any linkage with ENSO, we note that interpretation of tropical Atlantic SST in terms of a meridional dipole, as proposed by Servain (1991) , was recently reevaluated using alternative forms of spatial decomposition (see discussions in Enfield and Mayer 1997; Enfield et al. 1…”
BackgroundMethodInfluentialJanicot, S., & Fontaine, B. (1997) · doi:10.1016/s1251-8050(97)82512-8 · Cited by 12
Mendoza, D., Samaniego, E. P., Mora, D., Espinoza, M., & Campozano, L. (2018) · Climate Dynamics · doi:10.1007/s00382-018-4400-3 · Cited by 11
“2000; Servain 1991).”
A review of short-term climate variability mechanisms
Kayano, M. T., Rao, V. B., & Andreoli, R. V. (2005) · Advances in Space Research · doi:10.1016/j.asr.2004.10.010 · Cited by 8
Thermodynamic air-sea interactions and tropical atlantic SST dipole pattern
Li, L. (2001) · Physics and Chemistry of the Earth Part B Hydrology Oceans and Atmosphere · doi:10.1016/s1464-1909(00)00233-1 · Cited by 9
Moura, G. B. D. A., de Brito, J. I. B., de Sousa, F. D. A. S., Cavalcanti, E. P., da Silva, J. L. B., Nascimento, C., & Lopes, P. (2020) · doi:10.26848/rbgf.v13.4.p1463-1482 · Cited by 10
“As temperaturas nas áreas do Atlântico Tropical Norte (ATN) e Atlântico Tropical Sul (ATS) correspondem à região associada ao padrão de Dipolo do Atlântico Tropical (Moura & Shukla, 1981; Servain, 1991).”
BackgroundVariabilidade Interanual da Precipitação e Fluxo de Umidade Sobre a Amazônia Usando o QTCM
Sousa, A. C., Cândido, L. A., & Andreoli, R. V. (2018) · Revista Brasileira de Meteorologia · doi:10.1590/0102-7786331015 · Cited by 13
Tropical Atlantic Hurricanes, Easterly Waves, and West African Mesoscale Convective Systems
Kouadio, Y., Machado, L., & Servain, J. (2010) · doi:10.1155/2010/284503 · Cited by 10
“Positive and negative SST anomaly cores thus form an anomalous oceanic dipole, similar to the historical dipole studied many times in the past [35].”
BackgroundSelf-citationFontaine, B., Janicot, S., Moron, V., Roucou, P., & Trzaska, S. (1998) · La Météorologie · doi:10.4267/2042/47056 · Cited by 12
Neto, A. V. N., Giordani, H., Caniaux, G., & Araújo, M. (2018) · Journal of Geophysical Research Oceans · doi:10.1029/2017jc013436 · Cited by 10
“The other mode, first identified by Servain (1991) using principal component analysis, is characterized by an anomalous meridional SST gradient due to a north-south oscillation in SSTs.”
MethodOccurrence of Magellanic Penguins along the Northeast Brazilian Coast during 2008 Austral Winter
da Silva, R. R., Pereira, J., Tanajura, C., Lentini, C., Cirano, M., Boersma, P., & Rodrigues, R. (2012) · TheScientificWorldJournal · doi:10.1100/2012/686184 · Cited by 9
“Since the South Atlantic was cooler and the North Atlantic was warmer, the Atlantic SST dipole, coined by Servain [43], was positive for most of 2008.”
BackgroundKonda, M., Imasato, N., & Shibata, A. (1996) · doi:10.1007/bf02239462 · Cited by 9
“The negative correlation of SSTs in the northwest and the southeast tropical Atlantic as a dipole across the ITCZ has been inferred from the results of the empirical orthogonal function (EOF) analysis and principal component analysis (Weare, 1977; Moura and Shukla, 1981; Servain, 1991).”
Costa, R. L., Baptista, G., Gomes, H. B., Silva, F. D. S., da Rocha, R. L., & Nedel, A. (2021) · Anais da Academia Brasileira de Ciências · doi:10.1590/0001-3765202120190651 · Cited by 9
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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