Data and code associated with: The Permafrost and Organic LayEr module for Forest Models (POLE-FM) 1.0 ...

Abstract: Climate change and increased fire are eroding the resilience of boreal forests. This is problematic because boreal vegetation and the cold soils underneath store approximately 30% of all terrestrial carbon. Society urgently needs projections of where, when, and why boreal forests are most...

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Bibliographic Details
Main Authors: Hansen, Winslow, Foster, Adrianna, Gaglioti, Benjamin, Seidl, Rupert, Rammer, Werner
Format: Dataset
Language:unknown
Published: Cary Institute 2022
Subjects:
Online Access:https://dx.doi.org/10.25390/caryinstitute.21339090.v3
https://caryinstitute.figshare.com/articles/dataset/A_permafrost_and_soil-surface_organic_layer_module_for_simulating_high-latitude_forests_with_process-based_vegetation_models_/21339090/3
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Summary:Abstract: Climate change and increased fire are eroding the resilience of boreal forests. This is problematic because boreal vegetation and the cold soils underneath store approximately 30% of all terrestrial carbon. Society urgently needs projections of where, when, and why boreal forests are most likely to change. Permafrost (i.e., subsurface material that remains frozen for at least two consecutive years) and the thick soil-surface organic layers (SOLs) that insulate permafrost are important controls of boreal forest dynamics and carbon cycling. However, both are rarely included in the process-based vegetation models used to simulate future ecosystem trajectories. To address this challenge, we developed a new computationally efficient permafrost and SOL module that operates at fine spatial (1 ha) and temporal (daily) resolutions. The module mechanistically simulates daily changes in depth to permafrost, annual SOL accumulation, and their complex effects on boreal forest structure and functions. We coupled ...