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Simulating Impacts of Ice Storms on Forest Ecosystems
Published on: June 30, 2020
Improved simulation of poorly drained forests using Biome-BGC.
Ben Bond-Lamberty1, Stith T Gower, Douglas E Ahl
1Department of Forest Ecology and Management, University of Wisconsin, 1630 Linden Drive, Madison, WI 53706, USA. bpbond@wisc.edu
Tree Physiology
|February 3, 2007
Summary
This study modified the Biome-BGC forest model to better simulate poorly drained forests, improving its representation of biogeochemical cycling and bryophyte growth in these ecosystems.
Area of Science:
- Ecology
- Biogeochemistry
- Ecosystem Modeling
Background:
- Boreal and terrestrial biogeochemical cycling heavily rely on forested wetlands and peatlands.
- Existing forest process models are typically designed for upland systems, lacking accuracy for poorly drained environments.
Purpose of the Study:
- To enhance the Biome-BGC ecophysiological process model for improved simulation of poorly drained forests.
- To incorporate key hydrological and physiological processes specific to wetland conditions.
Main Methods:
- Modified Biome-BGC to include lateral water inflow, variable drainage, anoxic soil effects on decomposition, stomatal closure in flooded soils, and bryophyte growth.
- Parameterization of model changes using published data.
- Validation of ecosystem-level model performance against field data from the northern BOREAS site.
Main Results:
- Simulations showed reduced decomposition and vascular plant growth in poorly drained forests compared to well-drained ones.
- Integrated bryophyte photosynthetic response aligned with published data.
- Simulated net primary production, biomass, and soil carbon accumulation generally agreed with field measurements.
Conclusions:
- The modified Biome-BGC model offers improved simulation capabilities for poorly drained forests, particularly regarding bryophyte contributions and carbon cycling.
- Model sensitivity analyses highlighted oxygen restriction and stomatal closure as key factors influencing net primary production in these environments.
- The model's limitations include an inability to simulate true wetlands with prolonged flooding and associated processes like organic soil formation and water table dynamics.
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