Abstract

Abstract. Terrestrial ecosystems play a critical role in the global carbon cycle but have highly uncertain future dynamics. Ecosystem modeling that includes the scaling up of underlying mechanistic ecological processes has the potential to improve the accuracy of future projections while retaining key process-level detail. Over the past two decades, multiple modeling advances have been made to meet this challenge, such as the Ecosystem Demography (ED) model and its derivatives, including ED2 and FATES. Here, we present the global evaluation of the Ecosystem Demography model (ED v3.0), which, like its predecessors, features the formal scaling of physiological processes for individual-based vegetation dynamics to ecosystem scales, together with integrated submodules of soil biogeochemistry and soil hydrology, while retaining explicit tracking of vegetation 3-D structure. This new model version builds on previous versions and provides the first global calibration and evaluation, global tracking of the effects of climate and land-use change on vegetation 3-D structure, spin-up process and input datasets, as well as numerous other advances. Model evaluation was performed with respect to a set of important benchmarking datasets, and model estimates were within observational constraints for multiple key variables, including (i) global patterns of dominant plant functional types (broadleaf vs. evergreen), (ii) the spatial distribution, seasonal cycle, and interannual trends for global gross primary production (GPP), (iii) the global interannual variability of net biome production (NBP) and (iv) global patterns of vertical structure, including leaf area and canopy height. With this global model version, it is now possible to simulate vegetation dynamics from local to global scales and from seconds to centuries with a consistent mechanistic modeling framework amendable to data from multiple traditional and new remote sensing sources, including lidar.

Highlights

  • Terrestrial ecosystems and the associated carbon cycle are of critical importance in providing ecosystem services and regulating global climate

  • Quantification, attribution and future projections of the terrestrial carbon sink require an in-depth understanding of the underlying ecological processes and their sophisticated responses and feedbacks to climate change, elevated CO2, and land-use and land-cover change (LULCC) across mul

  • Major modifications in Ecosystem Demography (ED) v3.0 focus on four areas: plant functional type representation, leaf level physiology, hydrology and wood products

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Summary

Introduction

Terrestrial ecosystems and the associated carbon cycle are of critical importance in providing ecosystem services and regulating global climate. Tiple biomes and spatial and temporal scales (Canadell et al, 2007; Erb et al, 2013; Keenan and Williams, 2018) This demand for information has driven the emergence and development of dynamic global ecosystem models (DGVMs), which simplify the structure and functioning of global vegetation into several plant functional types and simulate vegetation distribution and associated biogeochemical and hydrological cycles with ecophysiological principles (Prentice et al, 2007; Prentice and Cowling, 2013). The evaluation included > 30 million grid cell pairs and > 103 forest inventory field plots This progression of development includes a range of model capabilities, spatial resolutions and evaluation data, spanning from coarse-resolution potential vegetation to high-spatialresolution contemporary conditions at regional scales. Multiple key variables are considered in the evaluation, including benchmark datasets on vegetation distribution, vegetation structure, and carbon and water fluxes

Methods
Model initialization and overview of experiments
Forcing data
Model evaluation
Vegetation distribution
Carbon fluxes
Carbon stocks
Water fluxes
Vegetation structure
Results
Evaluation of the PFT distribution
Evaluation of AGB and soil carbon
Evaluation of GPP, NBP and ET
Evaluation of canopy height and LAI vertical profile
Discussion and conclusions
Full Text
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