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Published on: September 12, 2017
Tree growth response to ENSO in Durango, Mexico
Marin Pompa-García1, Liliana Miranda-Aragón, Carlos Arturo Aguirre-Salado
1Facultad de Ciencias Forestales, Universidad Juárez del Estado de Durango, Av. Papaloapan y Blvd., Durango, Durango, 34120, Mexico, work.shapes@gmail.com.
El Niño-Southern Oscillation (ENSO) significantly influences Pinus cooperi tree growth in northwestern Mexico. Positive ENSO phases, or El Niño episodes, strongly correlate with increased radial growth in these forest ecosystems.
Area of Science:
- Ecology
- Climatology
- Dendrochronology
Background:
- Global forest dynamics are influenced by climatic teleconnections.
- El Niño-Southern Oscillation (ENSO) is a major driver of interannual climate variability, impacting regional climates.
- These climatic shifts can affect forest ecosystems, influencing plant phenology, growth, and extent.
Purpose of the Study:
- To investigate the impact of ENSO and regional microclimates on Pinus cooperi populations.
- To understand how P. cooperi growth responds to climatic variations in northwestern Mexico.
- To establish correlations between tree-ring data and ENSO events.
Main Methods:
- Dendrochronological techniques were employed to generate tree-ring chronologies (TRI).
- TRI data from 1950-2010 were correlated with ENSO and climate data.
- Multiple regressions were used to identify specific ENSO months directly influencing TRI.
Main Results:
- All five P. cooperi chronologies exhibited similar trends, indicating shared interannual growth variations.
- ENSO indices generally showed correspondence with tree-ring growth during synchronous periods.
- Positive ENSO values, corresponding to El Niño episodes, were found to drive radial growth.
Conclusions:
- ENSO demonstrates connectivity with the regional climate of northern Mexico.
- Radial growth of Pinus cooperi populations is significantly influenced by positive ENSO events.
- This study highlights the substantial impact of ENSO on forest ecosystems in the region.
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