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Interaction of Fire, Climate and Forest Structure in Northern MexicoWhat determines when forest fires will occur? Why do some forests burn more than others? How do El Niño and other climatic factors influence forest fires? Do widespread climate events or local characteristics, such as fuel, topography and ignition events, have the greatest effect on fire occurrence? These are questions we are trying to answer in this study focused on fire, climate, and forest structure in the mountains of northern Mexico. The project, funded by the National Science Foundation, will develop a new network of long fire and climate chronologies together with measurements of fuel dynamics in northern Mexico. We will incorporate a subset of unique relict sites where fire regimes and forest structures are least perturbed by human impacts over the nineteenth and twentieth centuries. We will reconstruct fire regimes for the past ±300 years using fire-scarred trees, species composition, age distribution, landscape patterns of forest stands, and historical records. Climate variables of precipitation, drought, El Niño-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), and Atlantic Multi-decadal Oscillation (AMO) patterns will be assessed with existing and new tree-ring and instrumental data sets. Forest structure (trees, regeneration, woody and litter debris) will be measured on gridded plots. These three long-term data sets will be applied to test the hypotheses that:
Last updated: November 18, 2007 |
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