Abstract

Abstract. Detection and quantification of greenhouse-gas emissions is important for both compliance and environment conservation. However, despite several decades of active research, it remains predominantly an open problem, largely due to model errors and assumptions that appear at each stage of the inversion processing chain. In 2015, a controlled-release experiment headed by Geoscience Australia was carried out at the Ginninderra Controlled Release Facility, and a variety of instruments and methods were employed for quantifying the release rates of methane and carbon dioxide from a point source. This paper proposes a fully Bayesian approach to atmospheric tomography for inferring the methane emission rate of this point source using data collected during the experiment from both point- and path-sampling instruments. The Bayesian framework is designed to account for uncertainty in the parameterisations of measurements, the meteorological data, and the atmospheric model itself when performing inversion using Markov chain Monte Carlo (MCMC). We apply our framework to all instrument groups using measurements from two release-rate periods. We show that the inversion framework is robust to instrument type and meteorological conditions. From all the inversions we conducted across the different instrument groups and release-rate periods, our worst-case median emission rate estimate was within 36 % of the true emission rate. Further, in the worst case, the closest limit of the 95 % credible interval to the true emission rate was within 11 % of this true value.

Highlights

  • Methane (CH4) is an important transition fuel for decarbonisation of the global energy system (International Energy Agency, 2017)

  • Convergence was assessed through visual inspection of the Markov chain Monte Carlo (MCMC) trace plots

  • In this article we have proposed a fully Bayesian model for atmospheric tomography that takes into account uncertainty in the data measurement process, the physical processes, and parameters appearing in the transport model, when estimating the emission rate

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Summary

Introduction

Methane (CH4) is an important transition fuel for decarbonisation of the global energy system (International Energy Agency, 2017). Cartwright et al.: Detection and quantification of methane emissions that its global warming potential is much greater than that of carbon dioxide (CO2), so that only a few percent of losses of CH4 into the atmosphere can negate any climate-change mitigation advantages from reducing conventional coal-fired power production (Kinnon et al, 2018) For this reason, it is critical that losses of CH4 along the supply chain are accurately accounted for to ensure public confidence in climatechange mitigation benefits of switching to natural gas. While ensemble inversions are frequently used to highlight the sensitivity of the results to atmospheric models and meteorological fields, learning unknown parameters associated with transport concurrently with the emission rate is not often done. This is largely due to the computational implications of such an approach.

The 2015 Ginninderra release experiment
Gaussian plume dispersion modelling
Low wind speeds
Predicted concentrations for point and path measurements
Bayesian atmospheric tomography
The data model
The process model
The parameter model
The precision parameters
The Gaussian plume model parameters
Bayesian inference
Observing system simulation experiment
Application to the Ginninderra data set
Sensitivity of results to model components
Conclusions
F1 E1 P1 BFEP1 B2 F2 E2 P2 BFEP2
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