Mem Inst Oswaldo Cruz, Rio de Janeiro, VOLUME 115 | JANUARY 2020
Original Article

Effects of El Niño-Southern Oscillation on human visceral leishmaniasis in the Brazilian State of Mato Grosso do Sul

Antonio Brandão da Silva Neto1,2, Everton Falcão de Oliveira1,2, César Claudio Cáceres Encina3, Helen Rezende de Figueiredo3, Antonio Conceição Paranhos Filho3, Alessandra Gutierrez de Oliveira1,2,+

1Universidade Federal de Mato Grosso do Sul, Programa de Pós-Graduação em Doenças Infecciosas e Parasitárias,  Faculdade de Medicina, Campo Grande, MS, Brasil
2Universidade Federal de Mato Grosso do Sul, Instituto de Biociências, Laboratório de Parasitologia Humana, Campo Grande, MS, Brasil
3Universidade Federal de Mato Grosso do Sul, Laboratório de Geoprocessamento para Aplicações Ambientais, Faculdade de Engenharias,  Arquitetura e Urbanismo e Geografia, Campo Grande, MS, Brasil

DOI: 10.1590/0074-02760190298
737 views 346 downloads

BACKGROUND Leishmaniases are considered a major public health problem in South America, specifically in Brazil. Moreover, the transmission and epidemiology of leishmaniasis are possibly associated with climatic and environmental variations.

OBJECTIVE This study aimed to assess the association between the extreme climatic phenomenon El Niño-Southern Oscillation (ENSO), the maximum and minimum variations of temperature, precipitation, and soil moisture and the incidence of visceral leishmaniasis (VL) in Mato Grosso do Sul (MS), Brazil, from 2002 to 2015.

METHODS The Niño 3.4 index was used for the ENSO variation. The other climatic data were obtained from the climatic tool TerraClimate. Records regarding VL were obtained from the Notification of Injury Information System.

FINDINGS From 2002 to 2015, there were 3,137 cases of VL recorded in MS. The annual incidence of the disease was negatively associated with the ENSO index and soil moisture in MS. The VL incidence increased during the negative phase of ENSO and decreased during the positive phase.

MAIN CONCLUSIONS The results demonstrated that the interannual cycles of incidence of human VL are significantly associated with the occurrence of the ENSO phenomenon and its phases, El Niño and La Niña.

Approximately 350 million people are at risk of Leishmania spp. protozoan infection, the second most common disease behind malaria that affects a signifi­cant number of people annually. Visceral leishmaniasis (VL) is considered the most severe clinical form of leish­maniases with a mortality rate of 90% if left untreated, specifically in children, elderly, and immunosuppressed patients. Leishmania parasites are transmitted through the bites of infected female sandflies.(1)

According to the World Health Organization, a total of 200,000-400,000 new cases of VL are reported, ac­counting for approximately 20,000 deaths annually.(1) In South America, approximately 95% of VL was recorded in Brazil. In 2013, the country registered more than a thousand human VL cases.(2)

The protozoan Leishmania infantum, an etiological agent of VL, is transmitted by Lutzomyia longipalpis and Lu. cruzi. The mode of transmission of L. infantum is con­sidered important to significantly understand the compo­nents of the epidemiological chain. In Brazil, VL might present different epidemiological profiles considering that the climatic characteristics, phytophysiognomic mosaics, and socioeconomic conditions of each region significantly vary.(3) Sandfly vectors are influenced by environmental variables. Temperature, rain, and moisture are the three major variables that influence sandflies’ biology. Higher than expected rainfall reduces the amount of the available nutrients for immature sandflies in the soil and increases soil moisture, limiting larvae and pupae development.(4, 5) On the contrary, higher temperatures and lower humidity levels lengthen the adult sandflies’ lifespan and promote female oviposition.(6)

Climate change possibly results in extreme weather events, which have been associated with the outbreaks of various infectious and parasitic diseases worldwide, such as cholera, malaria, dengue, and leishmaniasis.(7) Considering these extreme climatic events, the El Ni­ño-Southern Oscillation (ENSO) phenomenon, which consists of three phases, El Niño, La Niña, and neutral phase, should be emphasised. These phases are observed as a result of the anomalies in the sea surface tempera­ture (SST) of the Equatorial Pacific Ocean, which has a significant influence on the climate of the Americas. (8) The Pacific Ocean comprises the largest water mass on the planet; therefore, any variation in its temperature has a direct impact on the climate in different regions on Earth and can modify rainfall and temperature regimes.

Thus, ENSO may result in an above-average rainfall in one region, while it may cause extreme drought in an­other region, in addition to temperature anomalies, with cooler and warmer periods than normal.(8, 9)

Although climate changes are considered global phenomena, their effects vary according to region, and regional studies assessing the association between the epidemiology of VL and climate change are required in clinical practice. In MS, the transmission of VL has already been associated with different socioeconomic conditions;(10) however, the association between climate change and the occurrence of VL has not been deter­mined yet. Therefore, this is the first study conducted in Midwest Brazil that aimed to analyse the association between the extreme climatic phenomenon ENSO, the maximum and minimum variations of temperature, pre­cipitation, and soil moisture and the incidence of VL.


Study area - The State of Mato Grosso do Sul (MS) has an area of 357,145,534 km2. It is located in the mid­west region of Brazil and is bordered by Paraguay and Bolivia and the states of Paraná, São Paulo, Minas Gerais, Goiás, and Mato Grosso. The state comprises 79 municipalities, with Campo Grande as its capital city (Fig. 1). The state has an estimated 2,682,386 inhabit­ants, and according to the demographic census of 2010, 85.6% of the population live in an urban area.

According to the Köppen climate classification, there are three types of climate in MS - Aw (wet tropical climate with rainy season in summer and dry season in winter), Cfa (warm temperate climate with hot summer), and Cwa (humid temperate climate with dry winter and hot summer); the last one is restricted to the eastern end of the state. The average annual temperature and rainfall are approximately 25ºC and 1,500 mm, respectively. The majority of the vegetation of the state is composed of Cerrado lato sensu (tropical savanna-like climate); how­ever, Pantanal (wetland-like climate) areas in the west and Atlantic Forest areas in the south and southeast have been reported. The hydrographic basin comprises the Paraná and Paraguay rivers.(11)

Climatic data - We used the ENSO 3.4 index to as­sess the climatic phenomena. ENSO is calculated based on SST anomalies in the Niño 3.4 region, which com­prises the latitude 5ºN-5ºS and longitude 120º-170ºW, obtained from the latest version of the Extended Re­constructed Sea Surface Temperature version 4 sen­sor. ENSO data were obtained from the online platform available through the Climate Prediction Center, linked to the National Oceanic and Atmospheric Administra­tion of the United States. Positive and negative varia­tions are recorded from the average temperature history in the Equatorial Pacific. Anomalies less than -0.5ºC or greater than 0.5ºC for at least five consecutive months are considered cold phase/La Niña or warm phase/El Niño, respectively, whereas values in that interval (-0.5, 0.5) are considered the normal/neutral phase.(8)

The maximum temperature, minimum temperature, precipitation, and soil moisture data were obtained from the high-resolution dataset TerraClimate.(12) Using the free software program QGIS®, MS areas were divided, and the average values were obtained monthly for each year (2002-2015).(13)

Human visceral leishmaniasis cases - The records of VL cases from each MS municipality were obtained from the Notification of Grievance Information Sys­tem through the online platform of the Health Informa­tion System (TABNET-DATASUS) from 2002 to 2015. These data are in the public domain and are under the responsibility of the Ministry of Health.

Statistical analysis - First, the dataset was character­ised by the descriptive statistics of the variables of inter­est. The annual crude incidence of VL (per 100,000 in­habitants) was calculated for the state and municipalities with autochthonous reports during the study. Regarding the cumulative crude incidence of the whole period, 2002-2015, we considered the population in 2008 since this year represents half of the period under analysis.

The Shapiro-Wilk test was used to verify the as­sumption of the normal distribution of the variables.

Correlation analyses were used to confirm the asso­ciation between the incidence of VL and the independent variables (ENSO, maximum and minimum temperature, precipitation, and soil moisture). The Pearson correla­tion coefficient was used when the variables presented normal distribution and linear behaviour. In the absence of one of these characteristics, the Spearman correlation coefficient was used. To obtain an overview of the as­sociation between the variables under study, a dispersion and correlation matrix was constructed.

The level of significance was 5% (α = 0.05). The analy­ses were performed using the software R version 3.4.0.(14)


During the period of analysis (2002-2015), 3,137 cases of VL were recorded in 59 municipalities. We ob­served that the highest incidences were concentrated in the central region of the state, from east to west, pass­ing through Corumbá, Campo Grande, and Três Lagoas (Fig. 2). The highest number of VL cases was recorded in Campo Grande [1,774 (56%)], followed by Três La­goas [418 (13%)] and Aquidauana [129 (4%)] (Fig. 2A). However, when we analysed the incidence of VL, the highest incidence was noted in Três Lagoas (471.83 cases/100,000 inhabitants), followed by Rio Verde de Mato Grosso (418.17/100,000 inhabitants) and Anastácio (408.48/100,000 inhabitants) (Fig. 2B).




Table shows the annual VL distribution in MS (2002- 2015), ENSO variations, and El Niño and La Niña years. The highest numbers of VL were reported in 2012 (12.37 cases/100,000 inhabitants), 2011 (11.02 cases/100,000 inhabitants), and 2008 (10.83 cases/100,000 inhabitants). The lowest number of VL cases was reported in 2015, with 5.09 cases/100,000 inhabitants.

Fig. 3 shows the seasonal distribution of VL. The dis­ease was recorded in all months during the 14-year anal­ysis, with an average annual incidence of 0.899/100,000 inhabitants in January and a minimum of 0.725/100,000 inhabitants in June. Considering that the distribution of monthly incidence values does not have symmetrical distribution, in this case, the median represents the best measure of central tendency. Therefore, the months with the highest and lowest median incidence were March (0.864/100,000 inhabitants) and December (0.690/100,000 inhabitants), respectively. Generally, all the analysed var­iables presented oscillation during the evaluation period.

Fig. 4 shows the VL annual distribution and climatic series for MS from 2002 to 2015. Fig. 4A shows the annu­al incidence of VL (cases/100,000 inhabitants). Fig. 4B shows the ENSO variation using the Niño 3.4 index. Fig. 4C shows the maximum temperatures with the highest and lowest annual averages recorded in 2002 and 2010, respectively. Fig. 4D shows that that the highest and low­est annual averages for the minimum temperature were recorded in 2002 and 2008, respectively. Fig. 4E shows that the minimum and maximum precipitations were re­corded in 2002 and 2015, respectively, and Fig. 4F shows that the minimum and maximum values of soil moisture were recorded in 2002 and 2014, respectively.

Fig. 5 present the dispersion diagrams and corre­lation coefficients for the variables considered in our study. Within the variables analysed, only the incidence of VL had normal distribution, while all the climatic variables had non-normal distribution. Therefore, all analyses were performed based on Spearman correla­tion. The results obtained revealed that the annual in­cidence of VL was negatively associated with the mean ENSO variation (Niño 3.4) (r = -0.391, p < 0.001). When an increase in the ENSO mean was observed, a decrease in the incidence of VL was noted. Therefore, it can be observed that in the years with the highest VL incidence (2008, 2011, and 2012), a negative oscillation for ENSO, which was consistent with La Niña years, was recorded. While in the years with high ENSO averages, the inci­dence of VL decreased (5.09/100,000 inhabitants), spe­cifically in 2015, the year with the highest mean value (ENSO = 1.47), which was consistent with El Niño years.

A significant negative association was also observed between the incidence of VL and soil moisture (r = -0.181, p = 0.018), indicating the possibility of decreasing the par­asitic records in periods with more soaked soil (Fig. 4F). The statistical results of the other variables (i.e. the maxi­mum and minimum temperatures and precipitation) were insignificant (Fig. 4C-E). However, although the linear association between the incidence of VL and precipitation was i nsignificant (r = - 0.045, p = 0.564), a strong a sso­ciation was observed between the variables precipitation and soil moisture (r = 0.755, p < 0.001), indicating that humidity could directly influences precipitation, which is associated with the incidence of VL (Fig. 5). Based on the mean rainfall (Fig. 4E), a low incidence of VL during 2009, 2014, and 2015, years with high rainfall records and positive ENSO means, was also observed.


It seems that the spatial distribution pattern of VL cases in MS is concentrated in the same areas described by Antonialli et al.(10) from 1993 to 2004, with the highest incidence being reported on the east-west region of the state, from Corumbá to Três Lagoas. It can be noted that 20 municipalities (19 of them are located in the southern region of MS) had no available records of human VL cases from 2002 to 2015, indicating the probability that these areas do not present favorable conditions for VL development. Hence, future studies regarding sandfly diversity and parasite reservoirs and further investiga­tion on the possible underreported and asymptomatic human cases are required to confirm this hypothesis.

Despite the broad territory of the state and the epide­miological complexity of VL, our results demonstrated that the interannual cycles of VL incidence are possibly associated with the ENSO phenomenon. Although the La Niña effects on the state are insignificant in MS,(15) the association between infectious and parasitic diseas­es and ENSO has already been demonstrated in other countries. A study conducted in Panama indicated an increase in the occurrence of cutaneous leishmaniasis (CL) during the ENSO cold phase (La Niña).(16) In Ven­ezuela, between 1994 and 2003, a significant negative association between CL cases and ENSO was also ob­served. A significant number of CL cases were reported during the cold phase/La Niña; moreover, in that study, the authors observed that during the years where higher ENSO variation was observed, the incidence of CL was lower.(17) These studies are consistent with the result of our study regarding the association between the ENSO variation and the incidence of VL.

One of the probable factors involved in the variation of the number of VL cases in the present study is the fact that sandfly vectors are influenced by environmen­tal variables, such as temperature, humidity, luminosity, altitude, and vegetation cover.(18) Thus, these factors may also have an influence on the transmission of the para­site and consequently on VL development.

According to Marcuzzo and Oliveira,(15) El Niño events in MS result in increased maximum daily precipi­tation, while the La Niña phenomena have little influ­ence on the rainfall regime, which remains normal dur­ing the cold phase. Therefore, the reduction of VL cases in the state consistent with the occurrence of the El Niño phase may be due to a large volume of rainfall in a short period, resulting in soaked soil. Excessive moisture is a limiting factor for the evolution of immature stages (larvae and pupae) of sandflies that develop in the soil. (4) Although the incidence of VL showed no significant association with precipitation, it presented a negative as­sociation with soil moisture. Furthermore, soil moisture values showed a strong association with precipitation (r = 0,755, p < 0,001). It is worth mentioning that the lower incidences of VL were recorded during the years 2009, 2014, and 2015, where higher precipitation volumes were recorded. Therefore, it is believed that during the years with high precipitation and higher soil moisture, reduced VL cases are observed.

Queiroz et al.(5) cited that an above-average rainfall can reduce the organic matter available in the soil, pre­venting the immature sandflies’ development. Roger et al.(9) have shown, in French Guiana, that the mean an­nual number of cases of leishmaniasis (VL and CL) has a negative association with rainfall. Thus, during the El Niño years, which result in high maximum daily pre­cipitation in MS, limited immature sandfly development was observed. However, during the neutral and La Niña years, with normal rainfall, the ‘ideal’ moisture favoured vector development, enhancing vector transmission and consequently increasing VL cases.

On the contrary, in some regions worldwide, different associations between some diseases and the ENSO phe­nomenon are observed. In the region known as the Horn of Africa (Djibouti, Ethiopia, Eritrea, Somalia), El Niño events increase the risk of Rift Valley fever, cholera, and malaria, while La Niña increases the risk of dengue fever, chikungunya, and yellow fever.(19) However, it is worth emphasising that the vectors of these agents have differ­ent epidemiological profiles to that of sandflies.

In the Northeast region of Brazil, studies indicate that increased precipitation influences vector development. In that region, during or shortly after rainy periods, an increase in the number of VL cases and an increase in the population density of sandflies are observed.(20) The climatic differences between the northeast and central-west regions of Brazil might be the reason for this dis­crepancy between the results of the references above and the results in the present study. In the northeast, where the average temperature is normally high, El Niño results in drought and even higher temperatures. However, with the occurrence of La Niña, there is a decrease in this average temperature, enhancing vector development. In MS, the average rainfall and milder temperatures are considered the ideal conditions for sandflies’ dissemination.

Considering that the Pacific Ocean is the largest body of water on Earth, variations in its surface tem­perature are indicative of an increase or decrease in the planet’s thermal energy.(8) Thus, during El Niño, positive variations may indicate increased global temperature. Although there is no statistical evidence in the present study that confirms the association between the maxi­mum and/or minimum temperatures and the incidence of VL in the state, a negative association between the in­cidence of VL and ENSO was observed, which is in part an indirect measure of temperature. These results may be due to the temperature variables used, which were obtained based on the total MS area, including forest regions (Cerrado, Pantanal, and Atlantic Forest). There­fore, it is possible that when analysing only the urban­ised areas, where human infections are likely to occur, the temperature-VL association might be confirmed.

Temperatures up to 30ºC increase the reproduction of the vector insects — mosquitoes(19) and sandflies(21) — and decrease the maturation time of the pathogen in the vector. However, temperatures above this threshold may reduce insect survival due to fragility to desiccation. Females are significantly influenced by climatic variations, affecting their oviposition ability when temperatures are higher and humidity levels are lower.(6) Regarding the biology of Lu. longipalpis, a vector of L. infantum, Guzman and Tesh(22) have shown that temperatures approximately 18ºC nega­tively influence the immature forms (larvae and pupae) of sandflies, but the adult sandflies’ lifespan is higher. Thus, the exposure of individuals — hosts and reservoir — to the vectors can be increased. Rivas et al.(23) showed that at 30ºC, the maximum peak of the abundance of Lu. longi­palpis was considered lower than the other lower temper­ature regimes (20ºC and 25ºC). The studies cited above indicate that lower temperatures seem to favour sandfly reproduction and, consequently, lead to an increase in the number of VL cases. However, high temperatures, related to El Niño phases, do not favour sandfly reproduction, negatively affecting vector development. However, it is worth emphasising that there must be a threshold in the sandfly species for both low and high temperatures that either influences or not the survival of adult insects and the development of immature sandflies.

Murdock, Sternberg, and Thomas(24) have shown that even small changes in temperature can affect the dynam­ics of malaria transmission, indicating that an increment in temperature can reduce mosquitoes’ vector capac­ity by up to 89%. A similar pattern seems to influence sandflies as there is a decrease in the abundance of the species due to an increase in temperature.(16) Moreover, digestion, metabolic processes, and the development of different species of sandflies are significantly affected by ambient temperature.(25)

Moreover, the development of a parasite in a vector is also influenced by environmental conditions. Hlavaco­ca, Votypka, and Volf(26) showed that for the species Lu. longipalpis, temperatures lower than 20ºC allow the de­velopment, although slower, of the protozoan Leishma­nia peruviana. However, at 26°C, the infection rate and parasite load were significantly low. The authors suggest that lower temperatures delay the growth of the parasite after the blood meal; however, there is no impairment in its development in the sandfly’s gut. A similar result was observed for Phlebotomus papatasi, another sandfly species. The insects kept at 23ºC showed a higher rate of infection by Leishmania major compared to the dipter­ans kept at 28ºC. Moreover, lower temperatures increase the adult sandflies’ lifespan and prolong their digestion, allowing greater time for the development of infection. (25) These facts support the hypothesis that events such as El Niño, with higher temperatures and rainfall, are possibly associated with a decrease in the incidence of VL in MS, while its opposite events, La Niña and neutral phases, which have no influence on the climate in the MS, are associated with the increase in the occurrence of VL cases in the present study.

Considering climate changes will expectedly occur more frequently in the future, specifically the increase in global temperature, some authors suggest that the pat­tern of distribution of different diseases, such as VL, would possibly change.(7) In temperate areas, such as the regions in Europe and North America, an increase in number of vectors and VL cases are reported, confirm­ing that the distribution pattern of the parasite and its respective vectors has changed.(1, 27, 28)

Mathematical prediction indicates that with increas­ing global temperature, specifically in the tropical region, it is expected that there will be a decrease in the incidence rates of VL in this region since the vector insects would migrate to areas with higher altitude.(28, 29) Similar results were observed by Escobar et al.(7) in Ecuador, where the distribution of different insect vectors of arbovirus, leish­maniasis, malaria, and Chagas disease agents could be altered with the increase of atmospheric temperature. In this context, some authors stated that the increase in glob­al temperature tends to reduce the risk of vector-borne diseases, counteracting the negative effects of climate changes commonly associated with human health.(7, 29)

Finally, based on the monthly distribution of the in­cidence of VL, VL cases in all months of the 14-year analysis were recorded, consistent with the results of several studies regarding vectors observed in MS. The occurrence of Lu. longipalpis and Lu. cruzi in all months of the year in different regions of the state may explain the continuity of outbreaks of the disease during the year. Therefore, the presence of the vector can be used as a substitute to explain the occurrence of the disease through the annual course.(5, 18)

The variables studied in this research represent only a part of the factors that may influence the incidence of VL in MS. For example, deforestation and socioeco­nomic factors were not taken into consideration. Thus, further studies are required to evaluate the association between VL and different variables to better understand the aspects involved in the dynamics of the disease in the state. Environmental changes, urban migrations, basic sanitation, and the role of the reservoir in vari­ous clinical conditions are some of the factors that can facilitate the urbanisation of the VL. Failures regarding the notification of cases may also influence the number of cases of the disease in the state.(30) More sophisticated analytical methods incorporating temporal and spatial components simultaneously, such as regression models, can improve the understanding of the interrelationship between the links of the epidemiological chain. How­ever, the use of these approaches depends on the avail­ability and quality of the data.

One of the possible limitations in the present study was as follows: only the urbanised areas, where most of the VL cases are concentrated, were taken into consider­ation. The regional climatic variables were obtained for the MS region as a whole. Large forest areas, such as the Pantanal, may influence the values obtained for temper­ature (maximum and minimum), rainfall, and humidity. Thus, the most local analyses should be ideally obtained, contributing to the results presented here. Furthermore, studies assessing the association between ENSO and cli­mate change in MS are emerging, and only one reference was found,(15) indicating the possible effects of El Niño and La Niña events in the state.

In summary, the frequent occurrence of extreme cli­matic phenomena, such as El Niño and La Niña phases, may significantly influence the incidence of VL. El Niño reduces the incidence of VL and decreases the possible emergence of new VL cases probably due to the increase of rainfall volume and humidity affecting the vector’s biology. The possible effects of La Niña and the higher incidences of VL observed during these events need to be better evaluated to explain the parasite’s cycle in MS.


ABSN, EFO, ACPF and AGO - Conceptualisation, data analysis, and manuscript writing and review; CCCE - data analysis; HRF - conceptualisation and data analysis. The au­thors declare that the results of the manuscript are not plagia­rised and have not been published elsewhere.

01. WHO - World Health Organization. Weekly epidemiological record. 2017. Available from:
02. WHO - World Health Organization. Leishmaniasis: the vector. 2016. Available from:
03. Elkhoury ANSM, Alves WA, Gomes MLS, Sena JM, Luna EA. Visceral leishmaniasis in Brazil: trends and challenges. Cad Saude Publica. 2008; 24(12): 2941-7.
04. Lainson R. The American leishmaniasis: some observations on their ecology and epidemiology. R Soc Trop Med Hyg. 1982; 77: 569-96.
05. Queiroz MJA, Varjão JR, Moraes SC, Salcedo GE. Analysis of sandflies (Diptera: Psychodidae) in Barra do Garça, State of Mato Grosso, Brazil, and the influence of environmental variables on the vector density of Lutzomyia longipalpis (Lutz & Neiva, 1912). Rev Soc Bras Med Trop. 2012; 45(3): 313-7.
06. Brazil RP, Brazil BG. Biologia de flebotomíneos neotropicais. In: EF Rangel, Lainson R, editors. Flebotomíneos do Brasil. Rio de Janeiro: Fiocruz; 2003. p. 257-74.
07. Escobar LE, Romero-Allvarez D, Leon R, Lepe-Lopez MA, Craft ME, Borbor-Cordova MJ, et al. Declining prevalence of disease vectors under climate change. Sci Rep. 2016; 6(39150): 1-8.
08. NOAA/ESRL/PSD - National Oceanic and Atmospheric Administration/Earth System Research Laboratory/Physical Science Division. El Niño Southern Oscillation (ENSO). 2017. Available from:
09. Roger A, Nacher M, Hanf M, Drogoul AS, Adenis A, Basurko C, et al. Climate and leishmaniasis in French Guiana. Am J Trop Med Hyg. 2013; 89(3): 564-9.
10. Antonialli SAC, Torres TG, Paranhos Filho AC, Tolezano JE. Spatial analyses of American visceral leishmaniasis, in Mato Grosso do Sul State, Central-Brazil. J Infect. 2007; 54(5): 509-14.
11. Governo do Mato Grosso do Sul. Perfis de MS: Mato Grosso do Sul. 2016. Available from:
12. Abatzoglou JT, Dobrowski SZ, Parks SA, Hegewisch KC. Data descriptor: terraclimate, a high-resolution global dataset of monthly climate and climatic water balance from 1958-2015. Scient Data. 2018; 5(170191): 1-12.
13. QGIS - Development Team. QGIS Geographic Information System. Version 2.16.3 Nødebo. 2017. Available from:
14. R Core Team. R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. 2017. Available from: https://www.r-prpoject.org
15. Marcuzzo F, Oliveira NL. Impacto do El Niño e La Niña na precipitação máxima diária do Estado do Mato Grosso do Sul. Acta Geo. 2012; 6(13): 193-206.
16. Chaves LF, Calzada JE, Valderrama A, Saldaña A. Cutaneous leishmaniasis and sand fly fluctuations are associated with El Niño in Panamá. PLoS Negl Trop Dis. 2014; 8(10): e3210.
17. Cabaniel SG, Rada TL, Blanco GJJ, Morales AJR, Escalera AJP. Impacto de los eventos de El Niño Southern Oscillation (ENSO) sobre la leishmaniosis cutánea en Sucre, Venezuela, a través del uso de información satelital, 1994-2003. Rev Peru Med Exp Salud Publica. 2005; 22(1): 32-8.
18. Oliveira EF, Casaril AE, Fernandes WS, Ravanelli MS, Medeiros MJ, Gamarra RMA, et al. Monthly distribution of phlebotomine sand flies, and biotic and abiotic factors related to their abundance, in an urban area to which visceral leishmaniasis is endemic in Corumbá, Brazil. PLoS One. 2016; 11(10): e0165155.
19. Flahault A, Castaneda RR, Bolon I. Climate change and infectious diseases. Public Health Rev. 2016; 37(21): 1-3.
20. Lima ID, Lima ALM, Mendes-Aguiar CO, Coutinho JFV, Wilson ME, Pearson RD, et al. Changing demographics of visceral leishmaniasis in the northeast Brazil: lessons for the future. PLoS Negl Trop Dis. 2018; 12(3): e0006161.
21. Torres-Guerrero E, Quintanilla-Cedillo MR, Ruiz-Esmenjaud J, Arenas R. Leishmaniasis: a review. F1000Res. 2017; 6(750): 1-15.
22. Guzman H, Tesh RB. Effects of temperature and diet on the growth and longevity of phlebotomine sand flies (Diptera: Psychodidae). Biomedica. 2000; 20: 190-9.
23. Rivas GBS, Souza NA, Peixoto AA, Bruno RV. Effects of temperature and photoperiod on daily activity rhythms of Lutzomyia longipalpis (Diptera: Psychodidae). Parasit Vectors. 2014; 7(278): 1-9.
24. Murdock CC, Sternberg ED, Thomas MB. Malaria transmission potential could be reduced with current and future climate change. Sci Rep. 2016; 6(27771): 1-7.
25. Benkova I, Volf P. Effect of temperature on metabolism of Phlebotomus papatasi (Diptera: Psychodidae). J Med Entomol. 2007; 44: 150-4.
26. Hlavacoca J, Votypka J, Volf P. The effect of temperature on Leishmania (Kinetoplastida: Trypanosomatidae) development in sand flies. J Med Entomol. 2013; 50(5): 955-8.
27. Alten B, Maia C, Afonso MO, Campino L, Jiménez M, González E, et al. Seasonal dynamics of phlebotomine sand fly species proven vectors of Mediterranean leishmaniasis caused by Leishmania infantum. PLoS Negl Trop Dis. 2016; 10(2): e4458.
28. González C, Wang O, Strutz SE, Gonzáles-Salazar C, Sánchez-Cordero V, Sarkar S. Climate change and risk of leishmaniasis in North America: predictions from ecological niche models of vector and reservoir species. PLoS Negl Trop Dis. 2010; 4(1): e585.
29. González C, Paz A, Ferro C. Predicted altitudinal shifts and reduced spatial distribution of Leishmania infantum vector species under climate change scenarios in Colombia. Acta Trop. 2014; 129: 83-90.
30. Elkhoury ANSM, Carmo EH, Gomes MLS, Mota E. Análise dos registros de leishmaniose visceral pelo método de captura-recaptura. Rev Saude Publica. 2007; 41(6): 931-7.

Financial support: CAPES (Finance Code: 001), FUNDECT.
+ Corresponding author:
Received 12 August 2019
Accepted 22 January 2020

Citation: Silva Neto AB, Oliveira EF, Encina CCC, Figueiredo HR, Paranhos Filho AC, Oliveira AG. Effects of El Niño-Southern Oscillation on human visceral leishmaniasis in the Brazilian State of Mato Grosso do Sul. Mem Inst Oswaldo Cruz. 2020; 115: e190298.

Our Location

Memórias do Instituto Oswaldo Cruz

Av. Brasil 4365, Castelo Mourisco 
sala 201, Manguinhos, 21040-900 
Rio de Janeiro, RJ, Brazil

Tel.: +55-21-2562-1222

This email address is being protected from spambots. You need JavaScript enabled to view it.

Support Program


fiocruz governo
faperj cnpq capes