Abstract

Abstract. Accurate modelling of the carbon cycle strongly depends on the parametrization of its underlying processes. The Carbon Cycle Data Assimilation System (CCDAS) can be used as an estimator algorithm to derive posterior parameter values and uncertainties for the Biosphere Energy Transfer and Hydrology scheme (BETHY). However, the simultaneous optimization of all process parameters can be challenging, due to the complexity and non-linearity of the BETHY model. Therefore, we propose a new concept that uses ensemble runs and the adjoint optimization approach of CCDAS to derive the full probability density function (PDF) for posterior soil carbon parameters and the net carbon flux at the global scale. This method allows us to optimize only those parameters that can be constrained best by atmospheric carbon dioxide (CO2) data. The prior uncertainties of the remaining parameters are included in a consistent way through ensemble runs, but are not constrained by data. The final PDF for the optimized parameters and the net carbon flux are then derived by superimposing the individual PDFs for each ensemble member. We find that the optimization with CCDAS converges much faster, due to the smaller number of processes involved. Faster convergence also gives us much increased confidence that we find the global minimum in the reduced parameter space.

Highlights

  • The terrestrial biosphere plays an important role in the global carbon cycle and has a great impact on the accumulation of carbon dioxide (CO2) in the atmosphere

  • The study by Ziehn et al (2011a) has revealed that the performance of the optimization in Cycle Data Assimilation System (CCDAS) can be significantly improved if only the soil carbon parameters are constrained with atmospheric CO2 concentration data, while all parameters controlling net primary productivity (NPP) were kept fixed

  • Some parameters are constrained against data using the 4-D-Var data assimilation scheme, whereas the uncertainties of the remaining parameters are included via ensemble runs

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Summary

Introduction

The increase in the complexity of TEMs over recent years has led to an increase in the number of parameters. These issues arise due to the complexity and non-linearity of state-ofthe-art TEMs and the potentially high-dimensional parameter space In this contribution we address the convergence issue of the optimization scheme in the 4-D-Var approach as used in the Carbon Cycle Data Assimilation System (CCDAS) (Rayner et al, 2005) and propose a new concept for deriving the posterior PDF for parameters and target quantities in a global TEM. Soil moisture and leaf area index (LAI) fields are provided as inputs for a reduced version of BETHY, in the following referred to as CarbonBETHY This version is used to assimilate atmospheric CO2 concentration observations from a large number of observation stations for optimizing photosynthesis and soil carbon parameters and to derive their posterior uncertainties (Rayner et al, 2005; Scholze et al, 2007)

Data assimilation
Materials and methods
Challenges
Concept and test case
Findings
Conclusions
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