Effects of the El Niño - Southern Oscillation (ENSO) cycle on mosquito populations in southern California

2008 ◽  
Vol 33 (1) ◽  
pp. 17-29 ◽  
Author(s):  
David E. Heft ◽  
William E. Walton
2008 ◽  
Vol 136 (7) ◽  
pp. 2523-2542 ◽  
Author(s):  
Mark LaJoie ◽  
Arlene Laing

Abstract Cloud-to-ground (CG) lightning flashes from the National Lightning Detection Network are analyzed to determine if the El Niño–Southern Oscillation (ENSO) cycle influences lighting activity along the Gulf Coast region. First, an updated climatology of lightning was developed for the region. Flash density maps are constructed from an 8-yr dataset (1995–2002) and compared with past lightning climatologies. Second, lightning variability is compared with the phases of ENSO. Winter lightning distributions are compared with one published study of ENSO and lightning days in the Southeast. Flash density patterns are, overall, consistent with past U.S. lightning climatology. However, the peak flash density for the annual mean was less than observed in previous climatologies, which could be due to the disproportionately large percentage of cool ENSO periods compared to previous lightning climatologies. The highest annual lightning counts were observed in 1997, which consisted of mostly warm ENSO seasons; the 1997–98 El Niño was one of the strongest on record. The lowest lightning counts were observed in 2000, which had mostly cool or neutral phases of ENSO including the lowest Niño-3.4 anomaly of the study period. Analysis of winter season lightning flash densities substantiated the role of the ENSO cycle in winter season lightning fluctuations. Winter lightning activity increased dramatically during the 1997–98 El Niño. The lowest winter flash densities are associated with cool ENSO phases. Although 8 yr is inadequate to establish a long-term pattern, results indicate that ENSO influences lightning and that further study is warranted. As more years of lightning data are acquired, a more complete climatology can be developed.


Author(s):  
Holly Ching Yu Lam ◽  
Andy Haines ◽  
Glenn McGregor ◽  
Emily Ying Yang Chan ◽  
Shakoor Hajat

The El Niño Southern Oscillation (ENSO) is a major driver of climatic variability that can have far reaching consequences for public health globally. We explored whether global, regional and country-level rates of people affected by natural disasters (PAD) are linked to ENSO. Annual numbers of PAD between 1964–2017 recorded on the EM-DAT disaster database were combined with UN population data to create PAD rates. Time-series regression was used to assess de-trended associations between PAD and 2 ENSO indices: Oceanic Niño Index (ONI) and multivariate El Niño Index (MEI). Over 95% of PAD were caused by floods, droughts or storms, with over 75% of people affected by these three disasters residing in Asia. Globally, drought-related PAD rate increased sharply in El Niño years (versus neutral years). Flood events were the disaster type most strongly associated with El Niño regionally: in South Asia, flood-related PAD increased by 40.5% (95% CI 19.3% to 65.6%) for each boundary point increase in ONI (p = 0.002). India was found to be the country with the largest increase in flood-related PAD rates following an El Niño event, with the Philippines experiencing the largest increase following La Niña. Multivariate ENSO Index (MEI)-analyses showed consistent results. These findings can be used to inform disaster preparedness strategies.


2012 ◽  
Vol 40 (1-2) ◽  
pp. 109-121 ◽  
Author(s):  
Neil Berg ◽  
Alex Hall ◽  
Scott B. Capps ◽  
Mimi Hughes

2020 ◽  
Author(s):  
Elissa Yeates ◽  
Kayla Cotterman ◽  
Angela Rhodes

A non-stationary climate imposes considerable challenges regarding potential public health concerns. The El Niño Southern Oscillation (ENSO) cycle, which occurs every 2 to 7 years, correlates positively with occurrences of the waterborne disease cholera. The warm sea surface temperatures and extreme weather associated with ENSO create optimal conditions for breeding the Vibrio cholerae pathogen and for human exposure to the pathogenic waters. This work explored the impacts of ENSO on cholera occurrence rates over the past 50 years by examining annual rates of suspected cholera cases per country in relation to ENSO Index values. This study provides a relationship indicating when hydrologic conditions are optimal for cholera growth, and presents a statistical approach to answer three questions: Are cholera outbreaks more likely to occur in an El Niño year? What other factors impact cholera outbreaks? How will the future climate impact cholera incidence rates as it relates to conditions found in ENSO? Cholera outbreaks from the 1960s to the present are examined focusing on regions of Central and South America, and southern Asia. By examining the predictive relationship between climate variability and cholera, we can draw conclusions about future vulnerability to cholera and other waterborne pathogenic diseases.


2019 ◽  
Vol 12 (6) ◽  
pp. 2080
Author(s):  
Erika Collischonn ◽  
Bianca Marques Maio ◽  
Ricardo Brandolt

O El Niño/Oscilação Sul (ENOS) é uma oscilação conjunta oceano-atmosfera, que altera a Temperatura da Superfície do Mar (TSM), a pressão, o vento e a convecção tropical, principalmente no Oceano Pacífico, porém com reflexos na circulação atmosférica e no padrão de distribuição da precipitação em outras áreas do planeta, incluindo o sul do Brasil, conforme já comprovado por vários autores. Essa alteração de padrões pode aumentar o número de pessoas expostas a doenças, como a dengue, aumentando a probabilidade de surtos ou epidemias. Neste trabalho, o recorte temporal escolhido, de 2012 a 2017, abrange os dois anos em que mais casos de dengue autóctone ocorreram em Porto Alegre (2013 e 2016). Para o período, analisaram-se variabilidades a partir dos seguintes dados: Índice Niño 3.4 (NOAA); médias e totais mensais de elementos meteorológicos e as normais climatológicas 1981-2010 de Porto Alegre (WMO 83967- INMET); casos confirmados de dengue por semana epidemiológica e ano (SINAN-RS); dias com presença de jatos de baixos níveis (JBN) sobre Porto Alegre (Projeto Rios Voadores e INPE/CPTEC). A partir da organização destes dados, foi constatada uma correspondência entre o El Niño muito forte ocorrido em 2016, a presença quase constante dos JBN sobre Porto Alegre, precipitação bem superior à normal e o maior número de casos de dengue autóctone já registrado até então. Discute-se também as diferenças e semelhanças deste ano com o de 2013, que foi o segundo ano em registros de dengue autóctone.  Variability of Climate and Dengue Fever Cases in Porto Alegre/RS from 2012 to 2017 A B S T R A C TThe El Niño / Southern Oscillation (ENSO) The El Niño-Southern Oscillation (ENSO) cycle causes ripples through the global climate, changing air currents and rainfall patterns, The effect on the climate of southern Brazil was evidenced by several authors. The shifts in Niño years can increase the number of people exposed to a disease, such as dengue, increasing the likelihood of an outbreak. In this work, we analyzed a period of time that covers the two years in which more cases of autochthonous dengue fever occurred in Porto Alegre (2013 and 2016). For this period, variability was analyzed from the following data: Niño 3.4 (NOAA), monthly mean and cumulative meteorological data and climatological normal 1981/2010 of Porto Alegre (WMO 83967- INMET); confirmed cases of dengue fever per epidemiological week and per year (SINAN-RS); days with presence of low level jets (JBN) over Porto Alegre (INPE/CPTEC). The organization of these data showed correspondence between the very strong El Niño occurred in 2016, the almost constant presence of the JBN over Porto Alegre, the most intense and frequent precipitation, and the highest number of autochthonous dengue cases ever recorded. We also discuss the differences and similarities of this year with that of 2013, which was the second year in autochthonous dengue fever records.Keywords: El Niño, Low Lever Jet, precipitation, temperature, wind, dengue fever.


2012 ◽  
Vol 1 (1) ◽  
Author(s):  
Johnny Chavarría Viteri ◽  
Dennis Tomalá Solano

La variabilidad climática es la norma que ha modulado la vida en el planeta. Este trabajo demuestra que las pesquerías y acuicultura costera ecuatorianas no son la excepción, puesto que tales actividades están fuertemente influenciadas por la variabilidad ENSO (El Niño-Oscilación del Sur) y PDO (Oscilación Decadal del Pacífico), planteándose que la señal del cambio climático debe contribuir a esta influencia. Se destaca también que, en el análisis de los efectos de la variabilidad climática sobre los recursos pesqueros, el esfuerzo extractivo también debe ser considerado. Por su parte, la acción actual de la PDO está afectando la señal del cambio climático, encontrándose actualmente en fases opuestas. Se espera que estas señales entren en fase a finales de esta década, y principalmente durante la década de los 20 y consecuentemente se evidencien con mayor fuerza los efectos del Cambio Climático. Palabras Clave: Variabilidad Climática, Cambio Climático, ENSO, PDO, Pesquerías, Ecuador. ABSTRACT Climate variability is the standard that has modulated life in the planet. This work shows that the Ecuadorian  fisheries and aquaculture are not the exception, since such activities are strongly influenced by ENSO variability (El Niño - Southern Oscillation) and PDO (Pacific Decadal Oscillation), considering that the signal of climate change should contribute to this influence. It also emphasizes that in the analysis of the effects of climate variability on the fishing resources, the extractive effort must also be considered. For its part, the current action of the PDO is affecting the signal of climate change, now found on opposite phases. It is hoped that these signals come into phase at the end of this decade, and especially during the decade of the 20’s and more strongly evidencing the effects of climate change. Keywords: Climate variability, climate change, ENSO (El Niño - Southern Oscillation) and PDO  (Pacific Decadal Oscillation); fisheries, Ecuador. Recibido: mayo, 2012Aprobado: agosto, 2012


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