The climatic risk of Amazonian protected areas is driven by climate velocity until 2050.

Changes in species distribution in response to climate change might challenge the territorial boundaries of protected areas. Amazonia is one of the global regions most at risk of developing long distances between current and future analogous climates and the emergence of climate conditions without analogs in the past. As a result, species present within the network of Protected Areas (PAs) of Amazonia may be threatened throughout the 21st century. In this study, we investigated climate velocity based on future and past climate-analogs using forward and backward directions in the network of PAs of Amazonia, in order to assess the climatic risk of these areas to climate change and verify their effectiveness in maintaining the current climate conditions. Using current (1970-2000) and future (2041-2060) average annual air temperature and precipitation data with a resolution of 10 km, climate velocities across the entire Amazon biome and average climate velocities of PAs and Indigenous Lands (ILs) were evaluated. The results show that the effects of backward velocity will be greater than that of forward velocity in the Amazon biome. However, the PA network will be less exposed to backward velocity impacts than unprotected areas (UAs)-emphasizing the importance of these areas as a conservation tool. In contrast, for the forward velocity impacts, the PA network will be slightly more exposed than UAs-indicating that the current spatial arrangement of the PA network is still not the most suitable to minimize impacts of a possible climate redistribution. In addition, a large extent of no-analog climates for backward velocities was found in central Amazonia, indicating that high temperatures and changes in precipitation patterns in this region will surpass the historical variability of the entire biome, making it a potentially isolated and unsuitable climatic envelope for species in the future. Most of the no-analog climates are in PAs, however the climate risks in ILs should also be highlighted since they presented higher climate velocities than PAs in both metrics. Our projections contrast with the median latitudinal migration rate of 2 km/year observed in most ecosystems and taxonomic groups studied so far and suggest the need for median migration rates of 7.6 km/year. Thus, despite the important role of PAs and ILs as conservation tools, they are not immune to the effects of climate change and new management strategies, specific to each area and that allow adaptation to global changes, will be necessary.

Potential Distribution of Pilocarpus microphyllus in the Amazonia/Cerrado Biomes under Near-Future Climate Change Scenarios.

Pilocarpus microphyllus Stapf. ex Wardlew. (Rutaceae) is an endemic and threatened medicinal plant species from tropical Brazil. Popularly known as "jaborandi", it is the unique natural source of pilocarpine, an alkaloid used to medical treat glaucoma and xerostomia. Based on Species Distribution Models (SDMs), we modeled the suitability of P. microphyllus's geographical distribution considering three Global Circulation Models (GCMs) under two future climate change scenarios (SSP2-4.5 and SSP5-8.5). The quantitative analyses carried out using ten different SDM algorithms revealed that precipitation seasonality (Bio15) and precipitation of the driest month (Bio14) were the most important bioclimatic variables. The results evidenced four main key areas of continuous occurrence of the plant spreading diagonally over tropical Brazilian biomes (Amazon, Cerrado and Caatinga). The near-future (2020 to 2040) ensemble projections considering all GCMs and scenarios have indicated negative impacts for the potential loss or significant reduction in suitable habitats for P. microphyllus in the transition region between the Amazon and Cerrado into central and northern Maranhão state, and mainly in the Caatinga biome over the northern Piaui state. On the other hand, positive impacts of the expansion of the plant habitat suitability are projected over forest cover protected areas of the Amazon biome in the southeastern Pará state. Since the jaborandi is of socioeconomic importance for many families in the north/northeast Brazil, it is urgent to implement public policies for conservation and sustainable management, thus mitigating the impacts of global climate change.

Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America.

The oceanic South Atlantic Convergence Zone (SACZ) has played a major role during South America's 2021/2022 summer extreme rainy season, being responsible for more than 90% of the precipitation in some regions of Southeast Brazil and in some regions of the Southwestern Atlantic Ocean (SWA). The summer of 2021/2022 was unique and rare and considered an abnormally humid season as verified by official Brazilian Institutes. First, the unusual number of cases of SACZ episodes (seven), was the highest recorded in the last decade. Second, all the cases that occurred were oceanic SACZ that assumed characteristics of an Atmospheric River and produced an excessively anomalous amount of precipitation during this period. Excess precipitation along with the regions located in mountainous and very uneven relief, which by orographic effects favors high precipitation volumes, were responsible for amplifying the observed impacts, such as landslides and floods that caused several losses to society. We also showed the main effects of coupling and interaction between the waters of the surface layer of the SWA and the atmosphere. Our learning from this study ends with the unprecedented results of how the marine atmospheric boundary layer (MABL) is locally modulated by the sea surface temperature (SST) that lies just below it. Until the present moment, we emphasize that this important mechanism has not been widely highlighted in the literature, showing that even though the ocean is colder than before oceanic SACZ is established, it is still warmer than the overlying air, thus, the ocean continues to be an active source of heat and moisture for the atmosphere and enhances the MABL instability process.

[Seasonality of dengue reporting in state capitals in the Brazilian Amazon and impacts of El Niño/La Niña]. / Sazonalidade nas notificações de dengue das capitais da Amazônia e os impactos do El Niño/La Niña.

The dynamics of dengue transmission are multifactorial and involve socioeconomic, ecological, and environmental aspects, the latter being closely related to local climatic conditions that affect the vector's reproductive cycle. Climate depends in turn on tropical oceanic mechanisms such as phases of El Niño/La Niña over the Pacific. The study contributes to this discussion and reports on the correlations between the Multivariate ENSO Index (MEI) in the Pacific and the number of reported dengue cases in seven state capitals in the Brazilian Amazon from 2001 to 2012. The study also analyzes the seasonality pattern (quarterly mean values) in dengue cases throughout the region. Evidence that El Niño/La Niña causes a decrease versus increase in the local rainfall pattern is consistent with the lower versus higher number of reported dengue cases in most of the state capitals in the Amazon, a result proven by the statistically significant negative correlations seen in Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) and Palmas (Tocantins). The 12-years means (2001-2012) revealed the presence of pronounced seasonality in dengue incidence in the majority of the state capitals, with sharp peaks from January to March [Rio Branco (Acre), Manaus, Belém and Palmas] and from April to June (São Luís), corresponding to 50-70% of the annual total. State capitals farther north [Boa Vista (Roraima) and Macapá (Amapá)] showed dengue reporting in all quarters of the year, with no pronounced seasonality.

A dinâmica de transmissão da dengue é multifatorial e envolve aspectos socioeconômicos, ecológicos e ambientais, sendo este último intimamente relacionado às condições climáticas locais que interferem no ciclo reprodutivo dos vetores da doença. Por sua vez, o clima é dependente dos mecanismos oceânicos tropicais, a exemplo das fases de El Niño/La Niña sobre o Pacífico. O presente trabalho contribui com esta temática e reporta as correlações entre o índice MEI (Multivariate ENOS Index) do Pacífico e o número de casos notificados de dengue em sete capitais da Amazônia brasileira, no período de 2001 a 2012. Além disso, investiga-se o padrão de sazonalidade (médias trimestrais) dos casos de dengue ao longo da região. As evidências de que o fenômeno El Niño/La Niña provoca redução/aumento no padrão pluviométrico local é consistente com o número menor/maior de casos notificados de dengue na maior parte das capitais amazônicas, cujo resultado foi comprovado pelas correlações negativas estatisticamente significantes encontradas para Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) e Palmas (Tocantins). As médias dos 12 anos (2001/2012) revelaram a presença de sazonalidade pronunciada na incidência de dengue na maioria das capitais, com picos acentuados de janeiro a março [Rio Branco (Acre), Manaus, Belém e Palmas] e de abril a junho (São Luís), correspondendo em torno de 50% a 70% do total anual. As localidades mais ao norte [Boa Vista (Roraima) e Macapá (Amapá)] revelaram registro da dengue ao longo de todos os trimestres do ano, não apresentando sazonalidade acentuada.

La dinámica de transmisión del dengue es multifactorial e implica aspectos socioeconómicos, ecológicos y ambientales, estando estos últimos íntimamente relacionados con las condiciones climáticas locales que interfieren en el ciclo reproductivo de los vectores de la enfermedad. A su vez, el clima depende de los mecanismos oceánicos tropicales, como por ejemplo las fases de El Niño/La Niña sobre el Pacífico. El presente trabajo contribuye a esta temática e informa sobre las correlaciones entre el índice MEI (Multivariate ENOS Index) del Pacífico y el número de casos notificados de dengue en siete capitales de la Amazonia brasileña durante el período de 2001 a 2012. Además, se investiga el patrón de estacionalidad (medias trimestrales) de los casos de dengue a lo largo de la región. Las evidencias de que el fenómeno El Niño/La Niña provoca reducción/aumento en el patrón pluviométrico local es consistente con el número menor/mayor de casos notificados de dengue en la mayor parte de las capitales amazónicas, cuyo resultado se comprobó por las correlaciones negativas estadísticamente significativas encontradas en Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) y Palmas (Tocantins). Las medias de los doce años (2001/2012) revelaron la presencia de estacionalidad pronunciada en la incidencia de dengue en la mayoría de las capitales, con picos acentuados de enero a marzo [Rio Branco (Acre), Manaus, Belém y Palmas] y de abril a junio (São Luís), correspondiendo en torno del 50 al 70% del total anual. Las localidades más al norte [Boa Vista (Roraima) y Macapá (Amapá)] revelaron registro del dengue a lo largo de todos los trimestres del año, no presentando una estacionalidad acentuada.

Sazonalidade nas notificações de dengue das capitais da Amazônia e os impactos do El Niño/La Niña / Seasonality of dengue reporting in state capitals in the Brazilian Amazon and impacts of El Niño/La Niña / Estacionalidad en las notificaciones de dengue de las capitales de la Amazonia y los impactos de El Niño/La Niña

Resumo: A dinâmica de transmissão da dengue é multifatorial e envolve aspectos socioeconômicos, ecológicos e ambientais, sendo este último intimamente relacionado às condições climáticas locais que interferem no ciclo reprodutivo dos vetores da doença. Por sua vez, o clima é dependente dos mecanismos oceânicos tropicais, a exemplo das fases de El Niño/La Niña sobre o Pacífico. O presente trabalho contribui com esta temática e reporta as correlações entre o índice MEI (Multivariate ENOS Index) do Pacífico e o número de casos notificados de dengue em sete capitais da Amazônia brasileira, no período de 2001 a 2012. Além disso, investiga-se o padrão de sazonalidade (médias trimestrais) dos casos de dengue ao longo da região. As evidências de que o fenômeno El Niño/La Niña provoca redução/aumento no padrão pluviométrico local é consistente com o número menor/maior de casos notificados de dengue na maior parte das capitais amazônicas, cujo resultado foi comprovado pelas correlações negativas estatisticamente significantes encontradas para Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) e Palmas (Tocantins). As médias dos 12 anos (2001/2012) revelaram a presença de sazonalidade pronunciada na incidência de dengue na maioria das capitais, com picos acentuados de janeiro a março [Rio Branco (Acre), Manaus, Belém e Palmas] e de abril a junho (São Luís), correspondendo em torno de 50% a 70% do total anual. As localidades mais ao norte [Boa Vista (Roraima) e Macapá (Amapá)] revelaram registro da dengue ao longo de todos os trimestres do ano, não apresentando sazonalidade acentuada.

Abstract: The dynamics of dengue transmission are multifactorial and involve socioeconomic, ecological, and environmental aspects, the latter being closely related to local climatic conditions that affect the vector's reproductive cycle. Climate depends in turn on tropical oceanic mechanisms such as phases of El Niño/La Niña over the Pacific. The study contributes to this discussion and reports on the correlations between the Multivariate ENSO Index (MEI) in the Pacific and the number of reported dengue cases in seven state capitals in the Brazilian Amazon from 2001 to 2012. The study also analyzes the seasonality pattern (quarterly mean values) in dengue cases throughout the region. Evidence that El Niño/La Niña causes a decrease versus increase in the local rainfall pattern is consistent with the lower versus higher number of reported dengue cases in most of the state capitals in the Amazon, a result proven by the statistically significant negative correlations seen in Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) and Palmas (Tocantins). The 12-years means (2001-2012) revealed the presence of pronounced seasonality in dengue incidence in the majority of the state capitals, with sharp peaks from January to March [Rio Branco (Acre), Manaus, Belém and Palmas] and from April to June (São Luís), corresponding to 50-70% of the annual total. State capitals farther north [Boa Vista (Roraima) and Macapá (Amapá)] showed dengue reporting in all quarters of the year, with no pronounced seasonality.

Resumen: La dinámica de transmisión del dengue es multifactorial e implica aspectos socioeconómicos, ecológicos y ambientales, estando estos últimos íntimamente relacionados con las condiciones climáticas locales que interfieren en el ciclo reproductivo de los vectores de la enfermedad. A su vez, el clima depende de los mecanismos oceánicos tropicales, como por ejemplo las fases de El Niño/La Niña sobre el Pacífico. El presente trabajo contribuye a esta temática e informa sobre las correlaciones entre el índice MEI (Multivariate ENOS Index) del Pacífico y el número de casos notificados de dengue en siete capitales de la Amazonia brasileña durante el período de 2001 a 2012. Además, se investiga el patrón de estacionalidad (medias trimestrales) de los casos de dengue a lo largo de la región. Las evidencias de que el fenómeno El Niño/La Niña provoca reducción/aumento en el patrón pluviométrico local es consistente con el número menor/mayor de casos notificados de dengue en la mayor parte de las capitales amazónicas, cuyo resultado se comprobó por las correlaciones negativas estadísticamente significativas encontradas en Manaus (Amazonas), São Luís (Maranhão), Belém (Pará) y Palmas (Tocantins). Las medias de los doce años (2001/2012) revelaron la presencia de estacionalidad pronunciada en la incidencia de dengue en la mayoría de las capitales, con picos acentuados de enero a marzo [Rio Branco (Acre), Manaus, Belém y Palmas] y de abril a junio (São Luís), correspondiendo en torno del 50 al 70% del total anual. Las localidades más al norte [Boa Vista (Roraima) y Macapá (Amapá)] revelaron registro del dengue a lo largo de todos los trimestres del año, no presentando una estacionalidad acentuada.

Three decades of reference evapotranspiration estimates for a tropical watershed in the eastern Amazon.

This study estimated the reference evapotranspiration rate (ETo) for the Itacaiúnas River Watershed (IRW), Eastern Amazonia, and measured the accuracy of eight empirical equations: Penman-Monteith (PM), Priestley-Taylor (PT), Hargreaves and Samani (HS), Camargo (CAM), Thornthwaite (TH), Hamon (HM), Kharrufa (KF) and Turc (TC) using monthly data from 1980 to 2013. In addition, it verifies the regional applicability to the IRW using a for the Marabá-PA station. The methods TC and PM (FAO56) presented the best results, which demonstrate that radiation and higher temperatures are the dominant drivers in the Evapotranspiration process, while relative humidity and wind speed have a much smaller impact. The temporal and spatial variability of ETo for IRW show has strong seasonality, increasing during the dry season and decreasing during the rainy season. The statistical analyses at 1% level of significance, indicates that there is no correlation of the residuals between the dry and rainy seasons, and test of the physical parameters such as mean temperature, solar radiation and relative air humidity explains the variations of ETo.

Three decades of reference evapotranspiration estimates for a tropical watershed in the eastern Amazon

ABSTRACT This study estimated the reference evapotranspiration rate (ETo) for the Itacaiúnas River Watershed (IRW), Eastern Amazonia, and measured the accuracy of eight empirical equations: Penman-Monteith (PM), Priestley-Taylor (PT), Hargreaves and Samani (HS), Camargo (CAM), Thornthwaite (TH), Hamon (HM), Kharrufa (KF) and Turc (TC) using monthly data from 1980 to 2013. In addition, it verifies the regional applicability to the IRW using a for the Marabá-PA station. The methods TC and PM (FAO56) presented the best results, which demonstrate that radiation and higher temperatures are the dominant drivers in the Evapotranspiration process, while relative humidity and wind speed have a much smaller impact. The temporal and spatial variability of ETo for IRW show has strong seasonality, increasing during the dry season and decreasing during the rainy season. The statistical analyses at 1% level of significance, indicates that there is no correlation of the residuals between the dry and rainy seasons, and test of the physical parameters such as mean temperature, solar radiation and relative air humidity explains the variations of ETo.

Four decades of land-cover, land-use and hydroclimatology changes in the Itacaiúnas River watershed, southeastern Amazon.

Long-term human-induced impacts have significantly changed the Amazonian landscape. The most dramatic land cover and land use (LCLU) changes began in the early 1970s with the establishment of the Trans-Amazon Highway and large government projects associated with the expansion of agricultural settlement and cattle ranching, which cleared significant tropical forest cover in the areas of new and accelerated human development. Taking the changes in the LCLU over the past four decades as a basis, this study aims to determine the consequences of land cover (forest and savanna) and land use (pasturelands, mining and urban) changes on the hydroclimatology of the Itacaiúnas River watershed area of the located in the southeastern Amazon region. We analyzed a multi-decadal Landsat dataset from 1973, 1984, 1994, 2004 and 2013 and a 40-yr time series of water discharge from the Itacaiúnas River, as well as air temperature and relative humidity data over this drainage area for the same period. We employed standard Landsat image processing techniques in conjunction with a geographic object-based image analysis and multi-resolution classification approach. With the goal of detecting possible long-term trends, non-parametric Mann-Kendall test was applied, based on a Sen slope estimator on a 40-yr annual PREC, TMED and RH time series, considering the spatial average of the entire watershed. In the 1970s, the region was entirely covered by forest (99%) and savanna (∼0.3%). Four decades later, only ∼48% of the tropical forest remains, while pasturelands occupy approximately 50% of the watershed area. Moreover, in protected areas, nearly 97% of the tropical forest remains conserved, while the forest cover of non-protected areas is quite fragmented and, consequently, unevenly distributed, covering an area of only 30%. Based on observational data analysis, there is evidence that the conversion of forest cover to extensive and homogeneous pasturelands was accompanied by systematic modifications to the hydroclimatology cycle of the Itacaiúnas watershed, thus highlighting drier environmental conditions due to a rise in the region's air temperature, a decrease in the relative humidity, and an increase in river discharge.

Spatial and temporal variability of rainfall in eastern Amazon during the rainy season.

Empirical orthogonal functions (EOF) and composites analysis were employed on pentad data in order to investigate the tropical atmospheric-ocean patterns over the Atlantic Ocean and the spatial-temporal characteristics of the rainfall in eastern Amazon during the peak of the rainy season (February to April). The EOF results evidenced that the Intertropical Convergence Zone (ITCZ) is the main rainfall-producing system in eastern Amazon during the rainy season. Conditions associated with the southward SST gradient in the intertropical Atlantic formed the dynamic patterns that favored the position of the ITCZ to south of the equator, thus explaining the predominance of positive precipitation anomalies in eastern Amazon, especially in the state of Maranhão and northeastern Pará during the February and April months.

A ocorrência de malária em quatro municípios do estado do Pará, de 1988 a 2005, e sua relação com o desmatamento / Occurrence of malaria in four cities in the state of Pará during 1988 to 2005 and its relationships with deforestation

O objetivo deste trabalho foi estudar a ocorrência de malária em quatro diferentes regiões representativas do estado do Pará, buscando suas possíveis relações com as taxas de desmatamento. Foi realizado um estudo retrospectivo, com dados secundários, no período de 1988 a 2005, através de casos de malária registrados em quatro municípios do Estado (Anajás, Itaituba, Santana do Araguaia e Viseu), como também das taxas de desmatamento fornecidas pelo PRODES-INPE. Aplicou-se a técnica dos Quantis para se estabelecer cinco categorias ou classes de incidência da malária para cada município, sendo gerado posteriormente um IPA representativo para o Estado. De 1988 até 1994, as curvas de incidência de malária acompanham os números de desmatamento. A partir de 1995, evidenciaram-se anos consecutivos com altos índices de ocorrência da doença logo após os períodos de altas taxas de desmatamento, como registrado nos anos de 1995, 2000 e 2004. Percebeu-se que após a época de intenso desmatamento, os casos de malária variaram entre alto e muito alto no seu padrão de incidência, apontando que o desmatamento pode ser um fator de incremento na frequência e aumento no número de pessoas infectadas no estado do Pará.

The purpose of this paper is to study occurrence of malaria in four different regions of the state of Pará and its possible relationships with deforestation rates. A retrospective study using secondary data from 1988 to 2005, using malaria incidence records reported in four cities in the state (Anajás, Itaituba, Santana do Araguaia and Viseu), as well as deforestation rates provided by the PRODES-INPE. The quantiles method was applied to establish five categories or classes of malaria incidence for each city, and a state IPA was generated with the contributions of these cities. From 1988 to 1994, the curves of incidence of malaria follow deforestation rates. From 1995, there are consecutive years of high incidence levels after years of high deforestation rates, as registered in 1995, 2000 and 2004. It was noticed that after periods of intense deforestation the occurrence of malaria presented an incidence pattern between high and very high, suggesting that deforestation may be a factor in maintaining and increasing the number of cases in the state of Pará.

A Lagrangian identification of the main sources of moisture affecting northeastern Brazil during its pre-rainy and rainy seasons.

This work examines the sources of moisture affecting the semi-arid Brazilian Northeast (NEB) during its pre-rainy and rainy season (JFMAM) through a Lagrangian diagnosis method. The FLEXPART model identifies the humidity contributions to the moisture budget over a region through the continuous computation of changes in the specific humidity along back or forward trajectories up to 10 days period. The numerical experiments were done for the period that spans between 2000 and 2004 and results were aggregated on a monthly basis. Results show that besides a minor local recycling component, the vast majority of moisture reaching NEB area is originated in the south Atlantic basin and that the nearby wet Amazon basin bears almost no impact. Moreover, although the maximum precipitation in the "Poligono das Secas" region (PS) occurs in March and the maximum precipitation associated with air parcels emanating from the South Atlantic towards PS is observed along January to March, the highest moisture contribution from this oceanic region occurs slightly later (April). A dynamical analysis suggests that the maximum precipitation observed in the PS sector does not coincide with the maximum moisture supply probably due to the combined effect of the Walker and Hadley cells in inhibiting the rising motions over the region in the months following April.

On the influences of the El Niño, La niña and Atlantic Dipole Paterni on the Amazonian Rainfall during 1960-1998

The influence of the large-scale climatic variability dominant modes in the Pacific and in the Atlantic on Amazonian rainfall is investigated. The composite technique of the Amazon precipitation anomalies is used in this work. The basis years for these composites arc those in the period 1960-1998 with occurrences of extremes in the Southern Oscillation (El Niño or La Niña) and the north/south warm (or cold) sea surface temperature (SST) anomalies dipole pattern in the tropical Atlantic. Warm (cold) dipole means positive (negative) anomalies in the tropical North Atlantic and negative (positive) anomalies in the tropical South Atlantic. Austral summer and autumn composites for extremes in the Southern Oscillation (El Niño or La Niña) and independently for north/south dipole pattern (warm or cold) of the SST anomalies in the tropical Atlantic present values (magnitude and sign) consistent with those found in previous works on the relationship between Amazon rainfall variations and the SST anomalies in the tropical Pacific and Atlantic. However, austral summer and autumn composites for the years with simultaneous occurrences of El Niño and warm north/south dipole of the SST anomalies in the tropical Atlantic show negative precipitation anomalies extending eastward over the center-eastern Amazon. This result indicates the important role played by the tropical Atlantic in the Amazon anomalous rainfall distribution.

A influência dos modos dc variabilidade climática dc grande escala dominantes no Pacifico e Atlântico nas chuvas da Amazônia é investigada. A técnica de compósitos das anomalias dc precipitação na Amazônia é usada neste trabalho. Os anos base destes compósitos são aqueles do período 1960-1998 com ocorrências de extremos na Oscilação Sul (El Niño ou La Niña) e de padrão de dipolo norte/sul quente (ou frio) nas anomalias de TSM no Atlântico tropical. Dipolo quente (frio) significa anomalias positivas (negativas) no Atlântico tropical Norte e negativas (positivas) no Atlântico tropical Sul. Compósitos dc verão e outono austrais para extremos na Oscilação Sul (El Niño ou La Niña) e independente para padrão de dipolo norte/sul (quente ou frio) de anomalias de TSM no Atlântico tropical, apresentam valores (magnitude e signal) consistentes com aqueles encontrados cm trabalhos anteriores sobre a relação entre as variações de precipitação na Amazônia c anomalias de TSM no Pacífico e Atlântico tropicais. No entanto, compósitos dos verões e outonos austrais para os anos com ocorrências simultâneas de El Niño e dipolo quente norte/sul dc anomalias de TSM no Atlântico tropical mostram anomalias negativas de precipitação estendendo-se para leste sobre a Amazônia ccntro-leste. Este resultado indica o importante papel desempenhado pelo Atlântico tropical na distribuição anômala de precipitação na Amazônia.