Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico

This report addresses the following questions: a) is the diameter growth described by the standard ring width anomaly (SRWA) of Psudotsuga menziesii (Mirb.) Franco trees related to precipitation (P), pan evaporation (E), evapotranspiration (Et), runoff (Q), and soil moisture content (θ) derived from...

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Autores:
Návar, José
Lizárraga-Mendiola, Liliana
Tipo de recurso:
Article of journal
Fecha de publicación:
2014
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/73967
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/73967
http://bdigital.unal.edu.co/38444/
Palabra clave:
Recursos Naturales
Crecimiento de Arboles
mensuration
climate change
bioclimatic indexes
El Niño-Southern Oscillation
Pacific Decadal Oscillation
Atlantic Multidecadal Oscillation.
Hidrologia
Foresteria
Suelos
Climas
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
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oai_identifier_str oai:repositorio.unal.edu.co:unal/73967
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network_name_str Universidad Nacional de Colombia
repository_id_str
spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Návar, José58ce737b-c0d4-4424-af7b-b1a32cf337d3300Lizárraga-Mendiola, Lilianac58c89de-e573-4248-ac8b-b6a51be5172b3002019-07-03T17:07:01Z2019-07-03T17:07:01Z2014-03-26https://repositorio.unal.edu.co/handle/unal/73967http://bdigital.unal.edu.co/38444/This report addresses the following questions: a) is the diameter growth described by the standard ring width anomaly (SRWA) of Psudotsuga menziesii (Mirb.) Franco trees related to precipitation (P), pan evaporation (E), evapotranspiration (Et), runoff (Q), and soil moisture content (θ) derived from a water balance model?; b) is the SRWA associated with synoptic climate events such as El Nino Southern Oscillation (ENSO), the Pacific Decadal Oscillation (PDO), and the Atlantic Multidecadal Oscillation (AMO)?, and c) are P, Et and θ related to ENSO, PDO and AMO events? The SRWA for three dendrochronologies (Las Bayas and Banderas in Durango and El Gato in Zacatecas) from 1665 to 2001 addressed these questions. Instrumental measurements of P and E (1947-2007) and, using parameterized sub-models for the rainfall interception of Gash model (I) and Et, a mass balance approach evaluated Q and θ for a forest site near El Salto, Durango, Mexico. SRWA oscillations of several timescales had spectral peaks every 2-3; 3-7; and 9-12 years. The ENSO indices explained most of the total SRWA variation for all three chronologies (1990-2001). For the short (1990-2001) and middle-term (1945-2001) seasonal data, the SRWA variability was only linked to θ. The strength of the relationship weakened as the length of the time series increased, indicating that other variables control tree growth as well. The ENSO takes, on average, 4 to 8 months to display its effect on the hydrological variables and diameter growth in northern P. mensiezii trees of Mexico, making tree growth predictable.application/pdfspaUniversidad Nacional de Colombia, Facultad de Agronomía, Centro Editorialhttp://revistas.unal.edu.co/index.php/agrocol/article/view/41271Universidad Nacional de Colombia Revistas electrónicas UN Agronomía ColombianaAgronomía ColombianaAgronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 2357-3732 0120-9965Návar, José and Lizárraga-Mendiola, Liliana (2014) Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico. Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 2357-3732 0120-9965 .Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexicoArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTRecursos NaturalesCrecimiento de Arbolesmensurationclimate changebioclimatic indexesEl Niño-Southern OscillationPacific Decadal OscillationAtlantic Multidecadal Oscillation.HidrologiaForesteriaSuelosClimasORIGINAL41271-204404-1-PB.epubapplication/epub+zip567037https://repositorio.unal.edu.co/bitstream/unal/73967/1/41271-204404-1-PB.epub619fd02acc98142d8cdd6838c7b204c1MD5141271-202001-1-PB.pdfapplication/pdf841073https://repositorio.unal.edu.co/bitstream/unal/73967/2/41271-202001-1-PB.pdfb3450576187c4a15c7f72a7a9bfecf26MD52THUMBNAIL41271-202001-1-PB.pdf.jpg41271-202001-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg8560https://repositorio.unal.edu.co/bitstream/unal/73967/3/41271-202001-1-PB.pdf.jpg24f50c4991cedffe0f0c24effe8b794fMD53unal/73967oai:repositorio.unal.edu.co:unal/739672024-06-27 23:11:55.475Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
title Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
spellingShingle Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
Recursos Naturales
Crecimiento de Arboles
mensuration
climate change
bioclimatic indexes
El Niño-Southern Oscillation
Pacific Decadal Oscillation
Atlantic Multidecadal Oscillation.
Hidrologia
Foresteria
Suelos
Climas
title_short Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
title_full Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
title_fullStr Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
title_full_unstemmed Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
title_sort Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico
dc.creator.fl_str_mv Návar, José
Lizárraga-Mendiola, Liliana
dc.contributor.author.spa.fl_str_mv Návar, José
Lizárraga-Mendiola, Liliana
dc.subject.proposal.spa.fl_str_mv Recursos Naturales
Crecimiento de Arboles
mensuration
climate change
bioclimatic indexes
El Niño-Southern Oscillation
Pacific Decadal Oscillation
Atlantic Multidecadal Oscillation.
Hidrologia
Foresteria
Suelos
Climas
topic Recursos Naturales
Crecimiento de Arboles
mensuration
climate change
bioclimatic indexes
El Niño-Southern Oscillation
Pacific Decadal Oscillation
Atlantic Multidecadal Oscillation.
Hidrologia
Foresteria
Suelos
Climas
description This report addresses the following questions: a) is the diameter growth described by the standard ring width anomaly (SRWA) of Psudotsuga menziesii (Mirb.) Franco trees related to precipitation (P), pan evaporation (E), evapotranspiration (Et), runoff (Q), and soil moisture content (θ) derived from a water balance model?; b) is the SRWA associated with synoptic climate events such as El Nino Southern Oscillation (ENSO), the Pacific Decadal Oscillation (PDO), and the Atlantic Multidecadal Oscillation (AMO)?, and c) are P, Et and θ related to ENSO, PDO and AMO events? The SRWA for three dendrochronologies (Las Bayas and Banderas in Durango and El Gato in Zacatecas) from 1665 to 2001 addressed these questions. Instrumental measurements of P and E (1947-2007) and, using parameterized sub-models for the rainfall interception of Gash model (I) and Et, a mass balance approach evaluated Q and θ for a forest site near El Salto, Durango, Mexico. SRWA oscillations of several timescales had spectral peaks every 2-3; 3-7; and 9-12 years. The ENSO indices explained most of the total SRWA variation for all three chronologies (1990-2001). For the short (1990-2001) and middle-term (1945-2001) seasonal data, the SRWA variability was only linked to θ. The strength of the relationship weakened as the length of the time series increased, indicating that other variables control tree growth as well. The ENSO takes, on average, 4 to 8 months to display its effect on the hydrological variables and diameter growth in northern P. mensiezii trees of Mexico, making tree growth predictable.
publishDate 2014
dc.date.issued.spa.fl_str_mv 2014-03-26
dc.date.accessioned.spa.fl_str_mv 2019-07-03T17:07:01Z
dc.date.available.spa.fl_str_mv 2019-07-03T17:07:01Z
dc.type.spa.fl_str_mv Artículo de revista
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dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.eprints.spa.fl_str_mv http://bdigital.unal.edu.co/38444/
url https://repositorio.unal.edu.co/handle/unal/73967
http://bdigital.unal.edu.co/38444/
dc.language.iso.spa.fl_str_mv spa
language spa
dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/agrocol/article/view/41271
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Agronomía Colombiana
Agronomía Colombiana
dc.relation.ispartofseries.none.fl_str_mv Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 2357-3732 0120-9965
dc.relation.references.spa.fl_str_mv Návar, José and Lizárraga-Mendiola, Liliana (2014) Tree-ring growth and hydro-climatic variability in temperate dendrochronologies of northern mexico. Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 Agronomía Colombiana; Vol. 32, núm. 1 (2014); 103-112 2357-3732 0120-9965 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
Derechos reservados - Universidad Nacional de Colombia
http://creativecommons.org/licenses/by-nc/4.0/
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
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dc.publisher.spa.fl_str_mv Universidad Nacional de Colombia, Facultad de Agronomía, Centro Editorial
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