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Updated: Dec 7, 2025

Experimental Protocol for Manipulating Plant-induced Soil Heterogeneity
Published on: March 13, 2014
Local-scale Arctic tundra heterogeneity affects regional-scale carbon dynamics
M J Lara1,2,3, A D McGuire4, E S Euskirchen4
1Plant Biology Department, University of Illinois, Urbana, IL, 61801, USA. mjlara@illinois.edu.
Tundra landforms significantly impact carbon cycling. Accurately modeling Arctic ecosystems requires considering landscape heterogeneity at scales up to 4km², using at least two landform types to reduce uncertainty.
Area of Science:
- Geosciences
- Ecology
- Biogeochemistry
Background:
- Polygonal ground dominates northern Alaska's landscape (65%).
- Tundra landforms influence carbon and nutrient cycling at fine spatial scales.
- Current models often aggregate fine-scale heterogeneity into dominant land cover units for large-scale projections.
Purpose of the Study:
- To assess the impact of tundra heterogeneity on soil carbon dynamics across various spatial scales.
- To determine the necessary spatial scale and landform representation for accurate ecological modeling in the Arctic.
Main Methods:
- Utilized legacy data from Utqiaġvik, Alaska (1973-2016) for model initialization, parameterization, and validation.
- Employed process-based biogeochemical models to simulate soil carbon dynamics.
- Applied hierarchical cluster analysis to an ensemble of 21st-century simulations.
Main Results:
- Simulation uncertainty increased with reduced representation of tundra heterogeneity and coarser spatial scales.
- A minimum of two tundra landforms (dry and wet) and a maximum 4km² spatial scale were identified.
- Uncertainties were minimized to below 10% with appropriate scale and heterogeneity representation.
Conclusions:
- Fine-scale tundra heterogeneity is crucial for accurate soil carbon dynamics modeling.
- Regional to Pan-Arctic ecological models require explicit representation of landscape features.
- Optimizing model scale and heterogeneity is vital for reliable climate change impact projections.
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