Reconstrucción de la precipitación y caudal medio del río Piaxtla mediante anillos de crecimiento de Pseudotsuga menziesii (Mirb.) Franco

Díaz, José Villanueva; Gómez-Guerrero, Armando; Ávalos, Juan Estrada; Martínez-Sifuentes, Aldo Rafael

doi:10.21829/myb.2020.2631653

Cited by 4 publications

(6 citation statements)

References 56 publications

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“…Linking inter- and intra-annual variability with remote sensing data could provide finer resolution proxies for growth dynamics associated with climate variability that are still at an early stage. There are some studies dealing with the climatic drivers of tree growth and NDVI data in high-elevation forests from central Mexico (Correa-Díaz et al 2019 , 2020 ), and in semi-arid forests from northern Mexico and the south-western USA (Villanueva-Díaz et al 2009 ; Pompa-García et al 2013 ; González-Casares et al 2017 , 2020 ; Szejner et al 2020 ). However, intra-annual xylogenesis studies are still scarce in this region (but see Belmecheri et al 2018 ; Ziaco et al 2018 ; Pompa-García et al 2021 ).…”

Section: Introductionmentioning

confidence: 99%

Inter and intra-annual links between climate, tree growth and NDVI: improving the resolution of drought proxies in conifer forests

et al. 2021

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The inter- and intra-annual variability in radial growth reflects responses to climatic variability and water shortage, especially in areas subjected to seasonal drought. However, it is unknown how this variability is related to forest productivity, which can be assessed by measuring changes in canopy greenness and cover through remote sensing products as the Normalized Difference Vegetation Index (NDVI). We combine xylogenesis with measurements of inter-annual changes in seasonal wood production (earlywood width, adjusted latewood width) and NDVI to improve the understanding of climate and drought impacts on growth and forest productivity in a Pinus teocote stand located in northern Mexico. Cambial dynamics accelerated in March and a high production of radially enlarging and thickening tracheids were observed from April to October and from June to October, respectively. Tracheid maturation was very active in October when latewood production peaked. Wet conditions in winter-spring and summer-autumn enhanced earlywood and latewood production, respectively. Earlywood and latewood were constrained by long (4–10 months) and short (2–3 months) droughts, respectively. The earlywood production depended on April soil moisture, which agrees with the peak of radially enlarging tracheid production found during that month. Aligning drought proxies at inter- and intra-annual scales by using growth and productivity measures improves our understanding of conifer forest responses to water shortage.

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Section: Introductionmentioning

confidence: 99%

Inter and intra-annual links between climate, tree growth and NDVI: improving the resolution of drought proxies in conifer forests

et al. 2021

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“…The response of the tree-ring series to the runoff from November to July may be associated with a strong connection to the accumulated precipitation from the previous winter to spring (Table 2). This relationship has been well documented in the region [3,12,14,42,43]. Winter-spring precipitation in this region generally occurs at low intensity and often as snow, a situation that favors the process of water infiltration and accumulation in the soil profile.…”

Section: The Runoff Of the Gauge Station Las Burras And Its Correlati...mentioning

confidence: 84%

“…Before this period, historical archives documented the presence of severe droughts in the 1810s, 1790s, 1770s, 1750s, and 1720s [2]. Dendroclimatic reconstructions also detect intense droughts in previous periods such as the 1670s, 1570s, and 1490s [12][13][14], with severe impacts on forest ecosystems [15].…”

Section: Introductionmentioning

confidence: 99%

Tree Rings as Proxies of Historical Runoff in a National Park in Northern Mexico: A Major Ecosystem Service Provider

Villanueva-Díaz,

Correa-Díaz,

Castruita-Esparza

et al. 2023

Atmosphere

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A dendrochronological network of conifers (Pinus leiophylla, Pinus cembroides, Pinus engelmannii) was developed in the Cumbres de Majalca National Park (CMNP) in Chihuahua, Mexico, to reconstruct historical runoff patterns and examine the impact of ocean–atmosphere phenomena. The CMNP plays a vital role as a runoff source for Conchos River tributaries and groundwater recharge for Chihuahua City and nearby populations. The ring-width chronologies displayed a common signal from 1859 to 2021, with the highest association found between P. engelmannii and P. leiophylla (r = 0.65) and the lowest between P. cembroides and P. engelmannii (r = 0.55). The first principal component explained 75.7% of the variance, and among the species, P. leiophylla exhibited the highest correlation (0.624, p < 0.05) with the accumulated streamflow records from the previous November to July, allowing the construction of a bootstrapped model for runoff reconstruction. The reconstructed streamflow spanned from 1859 to 2014, with an average of 2.732 × 108 m3. Periods of low runoff occurred in 1860–1880, 1940–1960, and 1994–2014, while extreme wet years with high runoff occurred in 1865, 1884, and 1987. The interannual streamflow variability correlated significantly with ENSO indices (SOI, MEI, TRI, and sea surface temperature anomalies), particularly during the winter–spring seasons, indicating that warm phases of the ENSO increased precipitation and runoff. The analysis of return periods revealed probabilities for specific runoff volumes, enabling stakeholders to use the information to develop effective strategies for sustainable water allocation and utilization in the region.

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“…Para Q. sideroxyla, la respuesta a la variable precipitación fue similar a la de las coníferas de acuerdo a lo reportado por Villanueva Díaz et al (2009b) y por Chávez-Gándara et al (2017) en donde demostraron que la precipitación presente en el período invierno primavera, es la que mayormente impacta en el crecimiento de especies de coníferas, lo cual se explica a su vez por los tipos de bosque de pino-encino en donde se desarrollan, así mismo Ortiz-Quijano et al (2018), en un estudio desarrollado más al centro de México, obtuvieron valores significativos con la precipitación (R = 0.66, P < 0.01) presente de enero a junio, logrando identificar periodos de sequía y periodos de abundante precipitación en la cronología desarrollada para Fagus grandifolia subsp. mexicana.…”

Section: Discussionunclassified

Potencial dendroclimático del encino rojo, Quercus sideroxyla (Fagaceae) en México

Ortega-Arroyo

Jiménez-Pérez²,

Villanueva‐Díaz

et al. 2021

Rev. Biol. Trop.

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Introducción: Los estudios dendrocronológicos en México se han basado principalmente en las coníferas, mientras que las especies de madera dura han sido poco estudiadas. Este ha sido el caso del género Quercus, con una alta diversidad taxonómica en el país pero que no ha sido estudiado con fines dendrocronológicos, a pesar de los valores ecológicos y económicos de sus especies. Objetivo: En la presente investigación se determinó el potencial dendroclimático de Quercus sideroxyla en el noroeste de México, y su relación con variables climáticas como precipitación y temperatura. Métodos: La investigación se desarrolló en el estado de Durango en el ejido Chavarría Viejo en las coordenadas (23º43’ N & 105º33’ W), se recolectaron muestras de 5 a 7 cm en dos sitios bajo aprovechamiento forestal y se procesaron mediante técnicas dendrocronológicas convencionales. Resultados: Se desarrolló una cronología de ancho de anillo total, la cual se compuso por 30 muestras de 16 árboles para el período de 1917 a 2018 (101 años). Se obtuvieron valores de intercorrelación entre series de 0.43, de sensibilidad media de 0.36, relación señal-ruido de 3.53 y autocorrelación de primer orden (0.58). En cuanto a la relación clima-crecimiento, los valores de índice de ancho de anillo se correlacionaron con datos de la estación climática más cercana al sitio de estudio; donde la precipitación invierno-primavera (enero-mayo) fue la variable de mayor influencia en el crecimiento de la especie. Conclusiones: Con base en los parámetros dendrocronológicos se demuestra el alto potencial de la especie para ser empleada en estudios dendroclimáticos en la región, la respuesta de la especie a la precipitación es similar al de las coníferas con las que cohabita.

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Reconstrucción de la precipitación y caudal medio del río Piaxtla mediante anillos de crecimiento de Pseudotsuga menziesii (Mirb.) Franco

Cited by 4 publications

References 56 publications

Inter and intra-annual links between climate, tree growth and NDVI: improving the resolution of drought proxies in conifer forests

Inter and intra-annual links between climate, tree growth and NDVI: improving the resolution of drought proxies in conifer forests

Tree Rings as Proxies of Historical Runoff in a National Park in Northern Mexico: A Major Ecosystem Service Provider

Potencial dendroclimático del encino rojo, Quercus sideroxyla (Fagaceae) en México

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