Abstract

Abstract. Many applications in atmospheric science involve ill-posed inverse problems. A crucial component of many inverse problems is the proper formulation of a priori knowledge about the unknown parameters. In most cases, this knowledge is expressed as a Gaussian prior. This formulation often performs well at capturing smoothed, large-scale processes but is often ill equipped to capture localized structures like large point sources or localized hot spots. Over the last decade, scientists from a diverse array of applied mathematics and engineering fields have developed sparse reconstruction techniques to identify localized structures. In this study, we present a new regularization approach for ill-posed inverse problems in atmospheric science. It is based on Tikhonov regularization with sparsity constraint and allows bounds on the parameters. We enforce sparsity using a dictionary representation system. We analyze its performance in an atmospheric inverse modeling scenario by estimating anthropogenic US methane (CH4) emissions from simulated atmospheric measurements. Different measures indicate that our sparse reconstruction approach is better able to capture large point sources or localized hot spots than other methods commonly used in atmospheric inversions. It captures the overall signal equally well but adds details on the grid scale. This feature can be of value for any inverse problem with point or spatially discrete sources. We show an example for source estimation of synthetic methane emissions from the Barnett shale formation.

Highlights

  • Inverse problems are widespread in atmospheric sciences

  • The goal of this paper is to show how sparse reconstruction techniques can improve flux estimates in an atmospheric inverse modeling scenario

  • The present study is organized as follows: first, we briefly introduce the atmospheric inverse modeling problem in Sect

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Summary

Introduction

Inverse problems are widespread in atmospheric sciences. The estimation of greenhouse gas sources and sinks is a prime example. Numerous studies combine observations of greenhouse gas concentrations in the atmosphere and inverse modeling to infer sources and sinks at the Earth’s surface. Existing studies apply these techniques at municipal (e.g., Saide et al, 2011), regional (e.g., Zhao et al, 2009), continental (e.g., Miller et al, 2013), and global scales (e.g., Stohl et al, 2009). Inverse modeling estimates of greenhouse gas emissions are of scientific interest (e.g., to assess biospheric fluxes or improve process-based models). These estimates are key for monitoring and evaluating greenhouse gas emissions regulations (US National Research Council, 2010)

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