Climate trends and variability in Ecuador (1966–2011)

Descripción del Articulo

This study detects climate trends and variability from precipitation and temperature observations in Ecuador and assesses their links to the El Niño Southern Oscillation (ENSO) for the period 1966–2011, using the El Niño 1+2 and El Niño 3.4 indices. Excluding the Amazonian region (for which there is...

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Detalles Bibliográficos
Autores: Morán-Tejeda, E., Bazo, Juan, López-Moreno, J.I., Aguilar, E., Azorín-Molina, C., Sanchez‐Lorenzo, Arturo, Martínez, Rodney, Nieto, Juan J., Mejía, R., Martín‐Hernández, N., Vicente-Serrano, S.M.
Formato: artículo
Fecha de Publicación:2016
Institución:Servicio Nacional de Meteorología e Hidrología del Perú
Repositorio:SENAMHI-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.senamhi.gob.pe:20.500.12542/297
Enlace del recurso:https://hdl.handle.net/20.500.12542/297
https://doi.org/10.1002/joc.4597
Nivel de acceso:acceso abierto
Materia:ENSO
Precipitación
Temperatura
Zonas Costeras
Cuenca Hidrográfica
Clima
https://purl.org/pe-repo/ocde/ford#1.05.10
precipitacion - Clima y Eventos Naturales
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dc.title.en_US.fl_str_mv Climate trends and variability in Ecuador (1966–2011)
title Climate trends and variability in Ecuador (1966–2011)
spellingShingle Climate trends and variability in Ecuador (1966–2011)
Morán-Tejeda, E.
ENSO
Precipitación
Temperatura
Zonas Costeras
Cuenca Hidrográfica
Clima
https://purl.org/pe-repo/ocde/ford#1.05.10
precipitacion - Clima y Eventos Naturales
title_short Climate trends and variability in Ecuador (1966–2011)
title_full Climate trends and variability in Ecuador (1966–2011)
title_fullStr Climate trends and variability in Ecuador (1966–2011)
title_full_unstemmed Climate trends and variability in Ecuador (1966–2011)
title_sort Climate trends and variability in Ecuador (1966–2011)
author Morán-Tejeda, E.
author_facet Morán-Tejeda, E.
Bazo, Juan
López-Moreno, J.I.
Aguilar, E.
Azorín-Molina, C.
Sanchez‐Lorenzo, Arturo
Martínez, Rodney
Nieto, Juan J.
Mejía, R.
Martín‐Hernández, N.
Vicente-Serrano, S.M.
author_role author
author2 Bazo, Juan
López-Moreno, J.I.
Aguilar, E.
Azorín-Molina, C.
Sanchez‐Lorenzo, Arturo
Martínez, Rodney
Nieto, Juan J.
Mejía, R.
Martín‐Hernández, N.
Vicente-Serrano, S.M.
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Morán-Tejeda, E.
Bazo, Juan
López-Moreno, J.I.
Aguilar, E.
Azorín-Molina, C.
Sanchez‐Lorenzo, Arturo
Martínez, Rodney
Nieto, Juan J.
Mejía, R.
Martín‐Hernández, N.
Vicente-Serrano, S.M.
dc.subject.en_US.fl_str_mv ENSO
Precipitación
Temperatura
topic ENSO
Precipitación
Temperatura
Zonas Costeras
Cuenca Hidrográfica
Clima
https://purl.org/pe-repo/ocde/ford#1.05.10
precipitacion - Clima y Eventos Naturales
dc.subject.es_PE.fl_str_mv Zonas Costeras
dc.subject.none.fl_str_mv Cuenca Hidrográfica
Clima
dc.subject.ocde.none.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.05.10
dc.subject.sinia.none.fl_str_mv precipitacion - Clima y Eventos Naturales
description This study detects climate trends and variability from precipitation and temperature observations in Ecuador and assesses their links to the El Niño Southern Oscillation (ENSO) for the period 1966–2011, using the El Niño 1+2 and El Niño 3.4 indices. Excluding the Amazonian region (for which there is a lack of data), two main regions were distinguishable in terms of variability and trends among climate variables, especially for precipitation. In general, there was no trend in precipitation for the coastal region, and a very close relationship between the magnitude and seasonal distribution of precipitation and the El Niño 1+2 variability was found. In contrast, for the mountainous region (the Andes), there was an increase of precipitation during the study period, and a signal of El Niño 3.4 influence was detected. Temperatures were spatially homogeneous and showed an intense warming trend, except for maximum temperatures in the coastal region. The El Niño 1+2 influence on temperature was large from January to July. The results provide evidence of the close control exerted by the ENSO, especially in the coast of Ecuador, as well as for the occurrence of significant warming across the country independent of the ENSO phenomenon
publishDate 2016
dc.date.accessioned.none.fl_str_mv 2020-03-23T20:54:30Z
dc.date.available.none.fl_str_mv 2020-03-23T20:54:30Z
dc.date.issued.fl_str_mv 2016-01-15
dc.type.en_US.fl_str_mv info:eu-repo/semantics/article
dc.type.sinia.none.fl_str_mv text/publicacion cientifica
format article
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12542/297
dc.identifier.isni.none.fl_str_mv 0000 0001 0746 0446
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1002/joc.4597
dc.identifier.journal.none.fl_str_mv International Journal of Climatology
dc.identifier.url.none.fl_str_mv https://hdl.handle.net/20.500.12542/297
url https://hdl.handle.net/20.500.12542/297
https://doi.org/10.1002/joc.4597
identifier_str_mv 0000 0001 0746 0446
International Journal of Climatology
dc.language.iso.en_US.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:1097-0088
dc.rights.en_US.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
rights_invalid_str_mv Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América
http://creativecommons.org/licenses/by-nc-nd/3.0/us/
dc.format.none.fl_str_mv application/pdf
dc.coverage.spatial.none.fl_str_mv Andes
Ecuador
dc.publisher.en_US.fl_str_mv John Wiley and Sons Ltd
dc.source.en_US.fl_str_mv Repositorio Institucional - SENAMHI
Servicio Nacional de Meteorología e Hidrología del Perú
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instname_str Servicio Nacional de Meteorología e Hidrología del Perú
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spelling Morán-Tejeda, E.Bazo, JuanLópez-Moreno, J.I.Aguilar, E.Azorín-Molina, C.Sanchez‐Lorenzo, ArturoMartínez, RodneyNieto, Juan J.Mejía, R.Martín‐Hernández, N.Vicente-Serrano, S.M.AndesEcuador2020-03-23T20:54:30Z2020-03-23T20:54:30Z2016-01-15https://hdl.handle.net/20.500.12542/2970000 0001 0746 0446https://doi.org/10.1002/joc.4597International Journal of Climatologyhttps://hdl.handle.net/20.500.12542/297This study detects climate trends and variability from precipitation and temperature observations in Ecuador and assesses their links to the El Niño Southern Oscillation (ENSO) for the period 1966–2011, using the El Niño 1+2 and El Niño 3.4 indices. Excluding the Amazonian region (for which there is a lack of data), two main regions were distinguishable in terms of variability and trends among climate variables, especially for precipitation. In general, there was no trend in precipitation for the coastal region, and a very close relationship between the magnitude and seasonal distribution of precipitation and the El Niño 1+2 variability was found. In contrast, for the mountainous region (the Andes), there was an increase of precipitation during the study period, and a signal of El Niño 3.4 influence was detected. Temperatures were spatially homogeneous and showed an intense warming trend, except for maximum temperatures in the coastal region. The El Niño 1+2 influence on temperature was large from January to July. 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