scholarly journals Situation of Dengue after the Phenomenon of the Coastal El Niño

2020 ◽  
Author(s):  
Cristian Díaz-Vélez ◽  
Jorge Luis Fernández-Mogollón ◽  
John Alexis Cabrera-Enríquez ◽  
Stalin Tello-Vera ◽  
Oscar Medrano-Velásquez ◽  
...  
Keyword(s):  
El Niño ◽  
El Nino ◽  
Climatic Conditions ◽  
The Pacific ◽  
Weather Phenomenon ◽  
Peruvian Coast ◽  
Migratory Movement ◽  
The Pacific Ocean ◽  
Basic Infrastructure ◽  
Coastal El Niño

Coastal El Niño is a weather phenomenon that is caused by abnormal warming (above 0.4°C) of the Pacific Ocean waters near the coasts of Ecuador and Peru, and it can even reach the central and southern Peruvian coast. As a result of the climatic phenomenon, the Aedes aegypti vector (which in turn is a vector of chikungunya and Zika fever) had been quickly installed in 448 districts of Peru, and emergency was declared in 10 regions, which reported 231,874 victims; 1,129,013 affected and 143 dead. It is necessary to know this, because the direct impact of the weather phenomena contributes to the dengue vector conditioning, facilitating its dissemination with ease. The geographical and climatic conditions of the cities most affected by the El Niño Costero phenomenon turned them into zones of epidemics; in these places, there is an important population growth, from urbanization to sectorization in young towns and urban slums, where in many there is no basic infrastructure and water supply is insufficient, which requires temporary water storage, as well as high temperatures, migratory movement, and beaches with influx of people, which make not only dengue proliferate but also other arbovirosis such as chikungunya.

El Nino Chaos: Overlapping of Resonances Between the Seasonal Cycle and the Pacific Ocean-Atmosphere Oscillator

Science ◽  
1994 ◽  
Vol 264 (5155) ◽  
pp. 72-74 ◽  
Author(s):  
E. Tziperman ◽  
L. Stone ◽  
M. A. Cane ◽  
H. Jarosh
Keyword(s):  
Pacific Ocean ◽  
El Niño ◽  
Seasonal Cycle ◽  
El Nino ◽  
The Pacific ◽  
Ocean Atmosphere ◽  
The Pacific Ocean

scholarly journals El Niño–Southern Oscillation and Associated Climatic Conditions around the World during the Latter Half of the Twenty-First Century

2018 ◽  
Vol 31 (15) ◽  
pp. 6189-6207 ◽  
Author(s):  
Scott B. Power ◽  
François P. D. Delage
Keyword(s):  
El Niño ◽  
El Nino ◽  
Southern Oscillation ◽  
Precipitation Variability ◽  
Climatic Conditions ◽  
First Century ◽  
The Pacific ◽  
The World ◽  
Projected Changes ◽  
Mean State

Increases in greenhouse gas emissions are expected to cause changes both in climatic variability in the Pacific linked to El Niño–Southern Oscillation (ENSO) and in long-term average climate. While mean state and variability changes have been studied separately, much less is known about their combined impact or relative importance. Additionally, studies of projected changes in ENSO have tended to focus on changes in, or adjacent to, the Pacific. Here we examine projected changes in climatic conditions during El Niño years and in ENSO-driven precipitation variability in 36 CMIP5 models. The models are forced according to the RCP8.5 scenario in which there are large, unmitigated increases in greenhouse gas concentrations during the twenty-first century. We examine changes over much of the globe, including 25 widely spread regions defined in the IPCC special report Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation (SREX). We confirm that precipitation variability associated with ENSO is projected to increase in the tropical Pacific, consistent with earlier research. We also find that the enhanced tropical Pacific variability drives ENSO-related variability increases in 19 SREX regions during DJF and in 18 during JJA. This externally forced increase in ENSO-driven precipitation variability around the world is on the order of 15%–20%. An increase of this size, although substantial, is easily masked at the regional level by internally generated multidecadal variability in individual runs. The projected changes in El Niño–driven precipitation variability are typically much smaller than projected changes in both mean state and ENSO neutral conditions in nearly all regions.

scholarly journals El Niño arrives in the Pacific Ocean

Nature ◽  
2009 ◽  
Vol 460 (7253) ◽  
pp. 317-317
Keyword(s):  
Pacific Ocean ◽  
El Niño ◽  
El Nino ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals Meridional Extent and Interannual Variability of the Pacific Ocean Tropical–Subtropical Warm Water Exchange

2005 ◽  
Vol 35 (3) ◽  
pp. 323-335 ◽  
Author(s):  
Christopher S. Meinen
Keyword(s):  
Pacific Ocean ◽  
El Niño ◽  
El Nino ◽  
Warm Water ◽  
Height Anomaly ◽  
The South ◽  
El Niño Event ◽  
The Pacific ◽  
The Pacific Ocean ◽  
The Tropics

Abstract Altimetric observations of sea surface height anomaly (SSHA) from the TOPEX/Poseidon and ERS satellites, hydrography, and the ECMWF and Florida State University wind products are used to track warm water (≥20°C) as it is exchanged between the equatorial Pacific Ocean and the higher latitudes during 1993–2003. The large El Niño event of 1997–98 resulted in a significant discharge of warm water toward the higher latitudes within the interior of the Pacific Ocean. The exchange of anomalous warm water volume with the Northern Hemisphere appears to be blocked under the intertropical convergence zone, consistent with most current ideas on the time-mean tropical–subtropical exchange. Little of the warm water discharged northward across 5° and 8°N during the 1997–98 El Niño event could be traced as far as 10°N. To the south, however, these anomalous volumes of warm water were visible at least as far as 20°S, primarily in the longitudes around 130°–160°W. In both hemispheres most of the warm water appeared to flow westward before returning to the Tropics during the recharge phase of the El Niño–La Niña cycle. The buildup of warm water in the Tropics before the 1997–98 El Niño is shown to be fed primarily by warm water drawn from the region in the western Pacific within 5°S–15°N. The exchange cycle between the equatorial band and the higher latitudes north of the equator leads the cycle in the south by 6–8 months. These results are found in all three datasets used herein, hydrography, altimetric observations of SSHA, and Sverdrup transports calculated from multiple wind products, which demonstrates the robustness of the results.

Prospects for agriculture in 2017

2016 ◽  
Keyword(s):  
Pacific Ocean ◽  
El Nino ◽  
Extreme Weather ◽  
Extreme Weather Events ◽  
Content Type ◽  
Weather Events ◽  
The Pacific ◽  
Weather Phenomenon ◽  
Global Agriculture ◽  
The Pacific Ocean

Subject Prospects for agriculture in 2017. Significance The El Nino weather phenomenon, the heating of the Pacific Ocean, experienced through 2015 and 2016 was one of the strongest recorded, causing extreme weather events and decreasing global agriculture production. Next year promises a departure.

El Nino Episode Brews in the Pacific Ocean

Science News ◽  
1991 ◽  
Vol 140 (6) ◽  
pp. 87
Author(s):  
R. Monastersky
Keyword(s):  
Pacific Ocean ◽  
El Niño ◽  
El Nino ◽  
The Pacific ◽  
The Pacific Ocean

Interdecadal variability of El Niño onset and its impact on monsoon systems over areas encircling the Pacific Ocean

2016 ◽  
Vol 52 (12) ◽  
pp. 7173-7188 ◽  
Author(s):  
Jiaxi Cai ◽  
Jianjun Xu ◽  
Zhaoyong Guan ◽  
Alfred M. Powell
Keyword(s):  
Pacific Ocean ◽  
El Niño ◽  
El Nino ◽  
Interdecadal Variability ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals Análise dos Índices das Temperaturas Superficiais das Zonas Intertropicais dos Oceanos Pacífico e Atlântico associados às precipitações no Nordeste do Brasil

2021 ◽  
Vol 14 (2) ◽  
pp. 1081
Author(s):  
Beatriz Siqueira ◽  
Jonas Teixeira Nery ◽  
Oliver Messeguer-Ruiz
Keyword(s):  
Surface Temperature ◽  
El Niño ◽  
El Nino ◽  
South Atlantic ◽  
Northeast Brazil ◽  
The Pacific ◽  
The Pacific Ocean ◽  
Precipitation Anomalies ◽  
Temperature Indices ◽  
North And South

O objetivo deste estudo foi analisar, através de índices climáticos, a variabilidade da precipitação na região Nordeste do Brasil. Para tanto foram utilizados dados em ponto de grade para gerar o índice de precipitação, bem como dados da National Oceanic Atmospheric Administration (NOAA) para gerar os índices de temperatura do oceano Pacífico (setor EN3.4) e do oceano Atlântico tropical norte e sul. O período de análise foi de 1970 a 2012. Com base nesses índices foram realizadas correlações lineares de Pearson, entre o oceano Pacífico e o Atlântico tropical norte e o oceano tropical sul, na costa do Brasil. Anomalias de precipitação também foram calculadas para alguns anos de ocorrência do evento El Niño, denotando expressiva variabilidade de um evento para outro. De maneira geral, as correlações entre os índices envolvendo os referidos oceanos foram positivas e expressivas, o que permite considerar a influência dos oceanos na dinâmica das chuvas na área de estudo. A importância do Atlântico sul é mais nítida quando os índices de temperatura da superfície do mar apresentaram o mesmo sinal, tanto no Pacífico quanto no Atlântico, o que implica em correlações mais marcadas.Palavras-chave: Forçante climática, El Niño 3.4, Nordeste do Brasil, Atlântico tropical, Anomalias da precipitação.Analysis of Surface Temperature Indices of the Intertropical Zones of the Pacific and Atlantic Oceans associated with rainfall in Northeastern Brazil ABSTRACTThe objective of this study was to analyze, through climatic indices, the variability of precipitation in the Northeast region of Brazil. For that purpose, grid point data were used characterize the precipitation behaviour, as well as data from the National Oceanic Atmospheric Administration (NOAA) to determine the temperature of the Pacific Ocean (sector EN3.4) and the tropical North and South Atlantic Ocean. Based on these data, correlations were made, which are characterized as marked, between the dynamics of the Pacific Ocean and the dynamics of the tropical North and South Atlantic, directly influencing the precipitation regime in Northeast Brazil. Precipitation anomalies were also calculated for some years of the El Niño event, showing significant variability from one event to another. In general, the correlations between the indexes involving the referred oceans were positive and expressive, which allows considering the influence of the oceans on the dynamics of rainfall in the study area. The importance of the South Atlantic is clearer when the sea surface temperature indices show the same sign, both in the Pacific and in the Atlantic, which implies more marked correlations.Keywords: Climate forcing, El Niño 3.4, Northeast Brazil, Tropical Atlantic, Precipitation anomalies.

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