Abstract

AbstractForecasts of tropical ecosystem C cycling diverge among models due to differences in simulation of internal processes such as turnover, or transit times, of carbon pools. Estimates of these processes for the recent past are needed to test model representations, and so build confidence in model forecasts within and across biomes. Here, we evaluate carbon cycle process representation in two land surface models [Joint UK Land Environment Simulator (JULES) and Integrated Model of Land Surface Processes (INLAND)] for the period 2001–10 across Brazilian biomes. Model outputs are evaluated using the ILAMB system. Probabilistic benchmarking data were created using the carbon data model framework that assimilates observational times series of leaf area index and maps of woody biomass and soil C. New custom uncertainty metrics assess if models are within benchmark uncertainties. Simulations are better in homogeneous areas of vegetation type, and are less robust at ecotones between biomes, likely due to disturbance effects and parameter errors. Gross biosphere‐atmosphere fluxes are robustly modelled across Brazil. However, benchmark uncertainty is too high on net ecosystem exchange to provide an accurate evaluation of the models. The LSMs have significant differences in internal carbon allocation and the dynamics of the different C pools. JULES models dead C stocks more accurately while living C stocks are best resolved for INLAND. JULES' over‐estimate of the C wood pool results from over‐estimation of both inputs to wood and the transit time of wood. INLAND's under‐estimate of dead C stocks arises from an under‐estimate of the transit time of dead organic matter. The models are better at simulating annual averages than seasonal variation of fluxes. Analyses of monthly net C exchanges show that INLAND correctly simulates seasonality, but over‐estimates amplitudes, whereas JULES correctly simulates the annual amplitudes, but is out of phase with the benchmark.

Highlights

  • Tropical ecosystems, which cover 90% of Brazil, are major stores of carbon (C) and drivers of C exchanges between land and atmosphere

  • The analysis focuses on key biogenic stocks and fluxes to develop understanding of ecological process variation in time and space across Brazil

  • The analysis focused on the period 2001–2010, when outputs from Joint UK Land Environment Simulator (JULES), Integrated Model of Land Surface Processes (INLAND) and CARDAMOM were all available across Brazil

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Summary

Introduction

Tropical ecosystems, which cover 90% of Brazil, are major stores of carbon (C) and drivers of C exchanges between land and atmosphere. The response of these tropical ecosystems to increasing atmospheric CO2 concentrations and climate changes will have important feedbacks on the Earth system. Land surface models (LSMs) are used to predict future C cycling based on theorized carbon cycle climate feedbacks (Bonan, 2018). These models are complex, with multiple parameterized representations of interacting processes. The primary driver of this variability has been linked to model differences in the representation of slowly changing carbon cycle processes linked to transit times of C through the ecosystem (Hoffman et al, 2014)

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