4.7 Article

Accumulated Heating and Chilling Are Important Drivers of Forest Phenology and Productivity in the Algonquin-to-Adirondacks Conservation Corridor of Eastern North America

期刊

FORESTS
卷 12, 期 3, 页码 -

出版社

MDPI
DOI: 10.3390/f12030282

关键词

forest; phenology; productivity; temperature; random forest; partial dependence

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资金

  1. Ontario Research Fund (LOF grant) [22534]
  2. School of Environmental Studies, Queen's University
  3. Canada Foundation for Innovation

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Forest phenology and productivity in the Algonquin-to-Adirondacks conservation corridor of eastern North America have shown responsiveness to seasonal heating and chilling accumulation, predominantly driven by accumulated heating and chilling degree days. Although anthropogenic climate change has not triggered widespread changes in forest phenology and productivity in the area, the sensitivity of forest growth to inter-annual variation in seasonal temperature accumulation suggests potential future impacts of climate change on temperate forest areas as warming continues.
Research Highlights: Forest phenology and productivity were responsive to seasonal heating and chilling accumulation, but responses differed across the temperature range. Background and Objectives: Temperate forests have responded to recent climate change worldwide, but the pattern and magnitude of response have varied, necessitating additional studies at higher spatial and temporal resolutions. We investigated climatic drivers of inter-annual variation in forest phenology and productivity across the Algonquin-to-Adirondacks (A2A) conservation corridor of eastern North America. Methods: We used remotely sensed indices from the AVHRR sensor series and a suite of gridded climate data from the Daymet database spanning from 1989-2014. We used random forest regression to characterize forest-climate relationships between forest growth indices and climatological variables. Results: A large portion of the annual variation in phenology and productivity was explained by climate (R-p(2) > 80%), with variation largely driven by accumulated heating and chilling degree days. Only very minor relationships with precipitation-related variables were evident. Conclusions: Our results indicate that anthropogenic climate change in the A2A has not yet reached the point of triggering widespread changes in forest phenology and productivity, but the sensitivity of forest growth to inter-annual variation in seasonal temperature accumulation suggests that more temperate forest area will be affected by climate change as warming continues.

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