A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán
ABSTRACT : This paper analyzes the spatio-temporal variability of precipitation in western Iran by means of the Standardized Precipitation Index (SPI), calculated in annual and seasonal aggregations for wet and dry conditions over 46 synoptic stations with monthly data from 1957 to 2008. Regions of...
- Autores:
-
Cañón Barriga, Julio Eduardo
Biabanaki, Monireh
Eslamian, Saeid
Abedi Koupai, Jahangir
Boni, Giorgio
Gheysari, Mahdi
- Tipo de recurso:
- Article of investigation
- Fecha de publicación:
- 2014
- Institución:
- Universidad de Antioquia
- Repositorio:
- Repositorio UdeA
- Idioma:
- eng
- OAI Identifier:
- oai:bibliotecadigital.udea.edu.co:10495/34438
- Acceso en línea:
- https://hdl.handle.net/10495/34438
- Palabra clave:
- Irán
Iran
Análisis Espacio-Temporal
Spatio-temporal analysis
El Niño Oscilación del Sur
El Nino-Southern Oscillation
Análisis espectral
Spectrum analysis
ENSO
PDO
Standardized Precipitation Index (SPI)
- Rights
- openAccess
- License
- https://creativecommons.org/licenses/by/4.0/
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| dc.title.spa.fl_str_mv |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| title |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| spellingShingle |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán Irán Iran Análisis Espacio-Temporal Spatio-temporal analysis El Niño Oscilación del Sur El Nino-Southern Oscillation Análisis espectral Spectrum analysis ENSO PDO Standardized Precipitation Index (SPI) |
| title_short |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| title_full |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| title_fullStr |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| title_full_unstemmed |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| title_sort |
A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Irán |
| dc.creator.fl_str_mv |
Cañón Barriga, Julio Eduardo Biabanaki, Monireh Eslamian, Saeid Abedi Koupai, Jahangir Boni, Giorgio Gheysari, Mahdi |
| dc.contributor.author.none.fl_str_mv |
Cañón Barriga, Julio Eduardo Biabanaki, Monireh Eslamian, Saeid Abedi Koupai, Jahangir Boni, Giorgio Gheysari, Mahdi |
| dc.contributor.researchgroup.spa.fl_str_mv |
Grupo de Investigación en Gestión y Modelación Ambiental (GAIA) |
| dc.subject.decs.none.fl_str_mv |
Irán Iran Análisis Espacio-Temporal Spatio-temporal analysis El Niño Oscilación del Sur El Nino-Southern Oscillation |
| topic |
Irán Iran Análisis Espacio-Temporal Spatio-temporal analysis El Niño Oscilación del Sur El Nino-Southern Oscillation Análisis espectral Spectrum analysis ENSO PDO Standardized Precipitation Index (SPI) |
| dc.subject.lemb.none.fl_str_mv |
Análisis espectral Spectrum analysis |
| dc.subject.proposal.spa.fl_str_mv |
ENSO PDO Standardized Precipitation Index (SPI) |
| description |
ABSTRACT : This paper analyzes the spatio-temporal variability of precipitation in western Iran by means of the Standardized Precipitation Index (SPI), calculated in annual and seasonal aggregations for wet and dry conditions over 46 synoptic stations with monthly data from 1957 to 2008. Regions of homogeneous SPI realizations were delimited using principal components analysis (PCA) to highlight major variation modes distinguishable in the basin and singular spectrum analysis (SSA) was performed over the reconstructed values of SPI to identify their oscillation modes. Extreme SPI values associated with El Niño–Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) were also evaluated. Results show two significant oscillations around 4 and 8 years on the SPI with an increase in precipitation variability since 1990 and a tendency to have less rain during the cold season and more rain during the warm season. We calculated standardized products among SPI, ENSO, and PDO to determine years in which the indices reinforce each other, 1986, 1992, 1999, and 2008 being particularly significant in the associations. These results are important for water managers in western Iran because they indicate significant changes in precipitation regimes associated with ENSO and PDO signals that will help to assess the occurrence of droughts and floods in the area |
| publishDate |
2014 |
| dc.date.issued.none.fl_str_mv |
2014 |
| dc.date.accessioned.none.fl_str_mv |
2023-04-02T21:02:12Z |
| dc.date.available.none.fl_str_mv |
2023-04-02T21:02:12Z |
| dc.type.spa.fl_str_mv |
Artículo de investigación |
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http://purl.org/coar/resource_type/c_2df8fbb1 |
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https://purl.org/redcol/resource_type/ART |
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http://purl.org/coar/version/c_970fb48d4fbd8a85 |
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info:eu-repo/semantics/article |
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info:eu-repo/semantics/publishedVersion |
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http://purl.org/coar/resource_type/c_2df8fbb1 |
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| dc.identifier.citation.spa.fl_str_mv |
Biabanaki, Monireh & Eslamian, Saeid & Cañón, Julio & Boni, Giorgio & Gheysari, Mahdi. (2014). A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Iran. Hydrology Research. 45(2). 250. 10.2166/nh.2013.166. |
| dc.identifier.issn.none.fl_str_mv |
1998-9563 |
| dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/10495/34438 |
| dc.identifier.doi.none.fl_str_mv |
10.2166/nh.2013.166 |
| dc.identifier.eissn.none.fl_str_mv |
2224-7955 |
| identifier_str_mv |
Biabanaki, Monireh & Eslamian, Saeid & Cañón, Julio & Boni, Giorgio & Gheysari, Mahdi. (2014). A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Iran. Hydrology Research. 45(2). 250. 10.2166/nh.2013.166. 1998-9563 10.2166/nh.2013.166 2224-7955 |
| url |
https://hdl.handle.net/10495/34438 |
| dc.language.iso.spa.fl_str_mv |
eng |
| language |
eng |
| dc.relation.citationendpage.spa.fl_str_mv |
262 |
| dc.relation.citationissue.spa.fl_str_mv |
2 |
| dc.relation.citationstartpage.spa.fl_str_mv |
250 |
| dc.relation.citationvolume.spa.fl_str_mv |
45 |
| dc.relation.ispartofjournal.spa.fl_str_mv |
Hydrology Research |
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https://creativecommons.org/licenses/by/4.0/ |
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http://creativecommons.org/licenses/by/2.5/co/ |
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info:eu-repo/semantics/openAccess |
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https://creativecommons.org/licenses/by/4.0/ http://creativecommons.org/licenses/by/2.5/co/ http://purl.org/coar/access_right/c_abf2 |
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openAccess |
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14 |
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application/pdf |
| dc.publisher.spa.fl_str_mv |
IWA Publishing |
| dc.publisher.place.spa.fl_str_mv |
Londres, Inglaterra |
| institution |
Universidad de Antioquia |
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Cañón Barriga, Julio EduardoBiabanaki, MonirehEslamian, SaeidAbedi Koupai, JahangirBoni, GiorgioGheysari, MahdiGrupo de Investigación en Gestión y Modelación Ambiental (GAIA)2023-04-02T21:02:12Z2023-04-02T21:02:12Z2014Biabanaki, Monireh & Eslamian, Saeid & Cañón, Julio & Boni, Giorgio & Gheysari, Mahdi. (2014). A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western Iran. Hydrology Research. 45(2). 250. 10.2166/nh.2013.166.1998-9563https://hdl.handle.net/10495/3443810.2166/nh.2013.1662224-7955ABSTRACT : This paper analyzes the spatio-temporal variability of precipitation in western Iran by means of the Standardized Precipitation Index (SPI), calculated in annual and seasonal aggregations for wet and dry conditions over 46 synoptic stations with monthly data from 1957 to 2008. Regions of homogeneous SPI realizations were delimited using principal components analysis (PCA) to highlight major variation modes distinguishable in the basin and singular spectrum analysis (SSA) was performed over the reconstructed values of SPI to identify their oscillation modes. Extreme SPI values associated with El Niño–Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) were also evaluated. Results show two significant oscillations around 4 and 8 years on the SPI with an increase in precipitation variability since 1990 and a tendency to have less rain during the cold season and more rain during the warm season. We calculated standardized products among SPI, ENSO, and PDO to determine years in which the indices reinforce each other, 1986, 1992, 1999, and 2008 being particularly significant in the associations. These results are important for water managers in western Iran because they indicate significant changes in precipitation regimes associated with ENSO and PDO signals that will help to assess the occurrence of droughts and floods in the areaCOL000983214application/pdfengIWA PublishingLondres, Inglaterrahttps://creativecommons.org/licenses/by/4.0/http://creativecommons.org/licenses/by/2.5/co/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2A principal components/singular spectrum analysis approach to ENSO and PDO influences on rainfall in western IránArtículo de investigaciónhttp://purl.org/coar/resource_type/c_2df8fbb1https://purl.org/redcol/resource_type/ARThttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionIránIranAnálisis Espacio-TemporalSpatio-temporal analysisEl Niño Oscilación del SurEl Nino-Southern OscillationAnálisis espectralSpectrum analysisENSOPDOStandardized Precipitation Index (SPI)262225045Hydrology ResearchPublicationORIGINALCañonJulio_2014_APrincipalComponentsSingular.pdfCañonJulio_2014_APrincipalComponentsSingular.pdfArtículo de investigaciónapplication/pdf1104660https://bibliotecadigital.udea.edu.co/bitstreams/c5b8a382-0faf-48da-a39c-efd5d2fdd421/download797d88a1ffe3905d5d584390ead18769MD51trueAnonymousREADCC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8927https://bibliotecadigital.udea.edu.co/bitstreams/3025bf59-3164-4635-b62a-e90279a38de6/download1646d1f6b96dbbbc38035efc9239ac9cMD52falseAnonymousREADLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://bibliotecadigital.udea.edu.co/bitstreams/636cd037-e38b-44b3-8a51-90d86cdc07d0/download8a4605be74aa9ea9d79846c1fba20a33MD53falseAnonymousREADTEXTCañonJulio_2014_APrincipalComponentsSingular.pdf.txtCañonJulio_2014_APrincipalComponentsSingular.pdf.txtExtracted texttext/plain44936https://bibliotecadigital.udea.edu.co/bitstreams/9cbb51c2-b244-46c8-94d9-a214cdf176b8/download717e0dbe6dbc034767162dad54ea9158MD54falseAnonymousREADTHUMBNAILCañonJulio_2014_APrincipalComponentsSingular.pdf.jpgCañonJulio_2014_APrincipalComponentsSingular.pdf.jpgGenerated Thumbnailimage/jpeg13589https://bibliotecadigital.udea.edu.co/bitstreams/24c5f5a9-e7ff-44d8-8264-871629ec183f/download77ad3bf60beaa5f4a42f54939adf5fb8MD55falseAnonymousREAD10495/34438oai:bibliotecadigital.udea.edu.co:10495/344382025-03-26 21:04:59.051https://creativecommons.org/licenses/by/4.0/open.accesshttps://bibliotecadigital.udea.edu.coRepositorio Institucional de la Universidad de Antioquiaaplicacionbibliotecadigitalbiblioteca@udea.edu.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 |
