Abstract

Abstract. Assessing the uncertainties of simulation results of ecological models is becoming increasingly important, specifically if these models are used to estimate greenhouse gas emissions on site to regional/national levels. Four general sources of uncertainty effect the outcome of process-based models: (i) uncertainty of information used to initialise and drive the model, (ii) uncertainty of model parameters describing specific ecosystem processes, (iii) uncertainty of the model structure, and (iv) accurateness of measurements (e.g., soil-atmosphere greenhouse gas exchange) which are used for model testing and development. The aim of our study was to assess the simulation uncertainty of the process-based biogeochemical model LandscapeDNDC. For this we set up a Bayesian framework using a Markov Chain Monte Carlo (MCMC) method, to estimate the joint model parameter distribution. Data for model testing, parameter estimation and uncertainty assessment were taken from observations of soil fluxes of nitrous oxide (N2O), nitric oxide (NO) and carbon dioxide (CO2) as observed over a 10 yr period at the spruce site of the Höglwald Forest, Germany. By running four independent Markov Chains in parallel with identical properties (except for the parameter start values), an objective criteria for chain convergence developed by Gelman et al. (2003) could be used. Our approach shows that by means of the joint parameter distribution, we were able not only to limit the parameter space and specify the probability of parameter values, but also to assess the complex dependencies among model parameters used for simulating soil C and N trace gas emissions. This helped to improve the understanding of the behaviour of the complex LandscapeDNDC model while simulating soil C and N turnover processes and associated C and N soil-atmosphere exchange. In a final step the parameter distribution of the most sensitive parameters determining soil-atmosphere C and N exchange were used to obtain the parameter-induced uncertainty of simulated N2O, NO and CO2 emissions. These were compared to observational data of an calibration set (6 yr) and an independent validation set of 4 yr. The comparison showed that most of the annual observed trace gas emissions were in the range of simulated values and were predicted with a high certainty (Root-mean-squared error (RMSE) NO: 2.4 to 18.95 g N ha−1 d−1, N2O: 0.14 to 21.12 g N ha−1 d−1, CO2: 5.4 to 11.9 kg C ha−1 d−1). However, LandscapeDNDC simulations were sometimes still limited to accurately predict observed seasonal variations in fluxes.

Highlights

  • Trace gas emissions (N2O, nitric oxide (NO) and CO2) from soils of terrestrial ecosystems are highly variable in space and time due to the interplay of climatic drivers and various ecosystem processes involved in C and N transformation and associated production and consumptionPublished by Copernicus Publications on behalf of the European Geosciences Union.K.-H

  • We focus on the analysis of parameter-induced uncertainty quantification stemming from the soil-chemistry module describing all soil processes relevant for C and N trace gas production, consumption and transport, being crucial for the simulation of soil-atmosphere greenhouse gases (GHG) exchange

  • An estimate for the posterior distribution of the 26 most sensitive LandscapeDNDC parameters for simulation of soil N2O, NO and CO2 emissions was obtained by using Bayesian calibration technique and initial information on the likely range of the selected parameters

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Summary

Introduction

Trace gas emissions (N2O, NO and CO2) from soils of terrestrial ecosystems are highly variable in space and time due to the interplay of climatic drivers (mainly rainfall and temperature) and various ecosystem processes involved in C and N transformation and associated production and consumptionK.-H. An increasing number of biogeochemical models were tested on site scale and, after sound validation, were applied in a coupled GIS model approach for regionalisation of soil GHG emissions (Del Grosso et al, 2006; Kesik et al, 2006; Pathak et al, 2005; Li et al, 2004; Salas et al, 2007; Potter et al, 1996; Butterbach-Bahl et al, 2001; Kiese et al, 2005; Werner et al, 2007). The so-called Tier 3 approach includes up-scaling of GHG emissions, and the obligation to perform uncertainty quantification of the simulation results

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