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...
- 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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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 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ART |
format |
http://purl.org/coar/resource_type/c_6501 |
status_str |
publishedVersion |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/73967 |
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 |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
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 |
dc.format.mimetype.spa.fl_str_mv |
application/pdf |
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Universidad Nacional de Colombia, Facultad de Agronomía, Centro Editorial |
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Universidad Nacional de Colombia |
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