Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt
The present study evaluates the climatic response and the influence of ocean-atmosphere phenomena on the radial growth of Pinus hartwegii Lindl in Nevado de Colima (NEC), Nevado de Toluca (NET) and Pico de Orizaba (POR). Seventy-eight growth cores were dated, and their total ring width was measured....
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| Formaat: | Online |
| Taal: | spa |
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Instituto de Ecología, A.C.
2021
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| Online toegang: | https://myb.ojs.inecol.mx/index.php/myb/article/view/2276 |
| _version_ | 1799769421776945152 |
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| author | Manzanilla-Quiñones, Ulises Aguirre-Calderón , Oscar Alberto Villanueva-Díaz, José Martínez-Sifuentes, Aldo Rafael Delgado-Valerio, Patricia |
| author_facet | Manzanilla-Quiñones, Ulises Aguirre-Calderón , Oscar Alberto Villanueva-Díaz, José Martínez-Sifuentes, Aldo Rafael Delgado-Valerio, Patricia |
| author_sort | Manzanilla-Quiñones, Ulises |
| collection | MYB |
| description | The present study evaluates the climatic response and the influence of ocean-atmosphere phenomena on the radial growth of Pinus hartwegii Lindl in Nevado de Colima (NEC), Nevado de Toluca (NET) and Pico de Orizaba (POR). Seventy-eight growth cores were dated, and their total ring width was measured. Dating quality and chronology generation were performed in dendrochronological programs. Response analyses between dendrochronological series and climatic variables and the Niño Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO) and Atlantic Multidecadal Oscillation (AMO) indices were performed through Bootstrap correlations. Linear models were generated, calibrated, and verified through regression analysis, with which 57% and 53% of the instrumental variability of November-May precipitation for NEC (1940-2016) and December-May for NET (1928-2016) were reconstructed. The intense drought years of 1930, 1949, 1955, 1959, 1960, 1991, 1998, and 1999 and extreme wetness of 1992 coincided with the precipitation reconstructions for NEC and NET. Maximum temperature had a significant negative effect on radial growth of P. hartwegii at the three sites. The influence of ENSO on tree growth was significant (p<0.05) only at NEC. The influence of ODP and OMA was significant at all three sites (p<0.05). The local microenvironmental conditions where P. hartwegii develops in the three study sites modify the physiological response to climate and modulate the effect of ocean-atmospheric phenomena. |
| format | Online |
| id | oai:oai.myb.ojs.inecol.mx:article-2276 |
| institution | Madera y Bosques |
| language | spa |
| publishDate | 2021 |
| publisher | Instituto de Ecología, A.C. |
| record_format | ojs |
| spelling | oai:oai.myb.ojs.inecol.mx:article-22762022-11-29T22:17:49Z Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt Anillos de crecimiento de Pinus hartwegii como indicadores de fluctuaciones climáticas y de la influencia de fenómenos océano-atmósfera en la Faja Volcánica Transmexicana Manzanilla-Quiñones, Ulises Aguirre-Calderón , Oscar Alberto Villanueva-Díaz, José Martínez-Sifuentes, Aldo Rafael Delgado-Valerio, Patricia bosque de alta montaña dendrocronología índice de ancho de anillo precipitación reconstruida series de crecimiento variabilidad climática high mountain forest dendrochronology ring width index reconstructed precipitation growth series climatic variability The present study evaluates the climatic response and the influence of ocean-atmosphere phenomena on the radial growth of Pinus hartwegii Lindl in Nevado de Colima (NEC), Nevado de Toluca (NET) and Pico de Orizaba (POR). Seventy-eight growth cores were dated, and their total ring width was measured. Dating quality and chronology generation were performed in dendrochronological programs. Response analyses between dendrochronological series and climatic variables and the Niño Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO) and Atlantic Multidecadal Oscillation (AMO) indices were performed through Bootstrap correlations. Linear models were generated, calibrated, and verified through regression analysis, with which 57% and 53% of the instrumental variability of November-May precipitation for NEC (1940-2016) and December-May for NET (1928-2016) were reconstructed. The intense drought years of 1930, 1949, 1955, 1959, 1960, 1991, 1998, and 1999 and extreme wetness of 1992 coincided with the precipitation reconstructions for NEC and NET. Maximum temperature had a significant negative effect on radial growth of P. hartwegii at the three sites. The influence of ENSO on tree growth was significant (p<0.05) only at NEC. The influence of ODP and OMA was significant at all three sites (p<0.05). The local microenvironmental conditions where P. hartwegii develops in the three study sites modify the physiological response to climate and modulate the effect of ocean-atmospheric phenomena. El presente estudio evalúa la respuesta climática y la influencia de fenómenos océano-atmósfera sobre el crecimiento radial de Pinus hartwegii Lindl en el Nevado de Colima (NEC), Nevado de Toluca (NET) y Pico de Orizaba (POR). Se fecharon 78 núcleos de crecimiento, a los cuales se les midió el ancho de anillo total. La calidad del fechado y generación de cronologías se realizaron en los programas dendrocronológicos. Los análisis de respuesta entre series dendrocronológicas y variables climáticas e índices del Niño Oscilación del Sur (ENOS), Oscilación Decadal del Pacífico (ODP) y Oscilación Multidecadal del Atlántico (OMA) se realizaron a través de correlaciones Bootstrap. Mediante análisis de regresión se generaron, calibraron y verificaron modelos lineales, con los cuales se logró reconstruir 57% y 53% de la variabilidad instrumental de la precipitación de noviembre-mayo para NEC (1940-2016) y diciembre-mayo para NET (1928-2016). Los años de sequías intensas de 1930, 1949, 1955, 1959, 1960, 1991, 1998 y 1999 y de humedad extrema de 1992, coinciden con las reconstrucciones de precipitación para NEC y NET. La temperatura máxima tuvo un efecto negativo significativo en el crecimiento radial de P. hartwegii de los tres sitios. La influencia de ENOS sobre el crecimiento arbóreo fue significativo (p < 0.05) solamente en NEC. La influencia de ODP y OMA fue significativo en los tres sitios (p < 0.05). Las condiciones microambientales locales donde se desarrolla P. hartwegii en los tres sitios de estudio modifican la respuesta fisiológica al clima y modulan el efecto de los fenómenos océano-atmosféricos. Instituto de Ecología, A.C. 2021-12-30 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo evaluado por pares application/pdf text/xml https://myb.ojs.inecol.mx/index.php/myb/article/view/2276 10.21829/myb.2021.2732276 Madera y Bosques; Vol. 27 No. 3 (2021): Autumn 2021; e2732276 Madera y Bosques; Vol. 27 Núm. 3 (2021): Otoño 2021; e2732276 2448-7597 1405-0471 spa https://myb.ojs.inecol.mx/index.php/myb/article/view/2276/2320 https://myb.ojs.inecol.mx/index.php/myb/article/view/2276/2365 10.21829/myb.2018.243556 10.21829/myb.2019.252663 http://creativecommons.org/licenses/by-nc-sa/4.0 |
| spellingShingle | Manzanilla-Quiñones, Ulises Aguirre-Calderón , Oscar Alberto Villanueva-Díaz, José Martínez-Sifuentes, Aldo Rafael Delgado-Valerio, Patricia Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title | Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title_full | Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title_fullStr | Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title_full_unstemmed | Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title_short | Tree-rings of Pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the Transmexican Volcanic Belt |
| title_sort | tree-rings of pinus hartwegii as indicators of climatic fluctuations and the influence of ocean-atmosphere phenomena in the transmexican volcanic belt |
| url | https://myb.ojs.inecol.mx/index.php/myb/article/view/2276 |
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