A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion

Atmospheric inversions are frequently used to estimate fluxes of atmospheric greenhouse gases (e.g., biospheric CO<sub>2</sub> flux fields) at Earth's surface. These inversions typically assume that flux departures from a prior model are spatially smoothly varying, which are then mo...

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Main Authors: J. Ray, J. Lee, V. Yadav, S. Lefantzi, A. M. Michalak, B. van Bloemen Waanders
Format: Article
Language:English
Published: Copernicus Publications 2015-04-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/8/1259/2015/gmd-8-1259-2015.pdf
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spelling doaj-22ddc369a4374e33ba1b082039a1a26c2020-11-24T23:49:24ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032015-04-01841259127310.5194/gmd-8-1259-2015A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversionJ. Ray0J. Lee1V. Yadav2S. Lefantzi3A. M. Michalak4B. van Bloemen Waanders5Sandia National Laboratories, P.O. Box 969, Livermore, CA 94551, USASandia National Laboratories, P.O. Box 969, Livermore, CA 94551, USACarnegie Institution for Science, Stanford, CA 94305, USASandia National Laboratories, P.O. Box 969, Livermore, CA 94551, USACarnegie Institution for Science, Stanford, CA 94305, USASandia National Laboratories, P.O. Box 5800, Albuquerque, NM 87185-0751, USAAtmospheric inversions are frequently used to estimate fluxes of atmospheric greenhouse gases (e.g., biospheric CO<sub>2</sub> flux fields) at Earth's surface. These inversions typically assume that flux departures from a prior model are spatially smoothly varying, which are then modeled using a multi-variate Gaussian. When the field being estimated is spatially rough, multi-variate Gaussian models are difficult to construct and a wavelet-based field model may be more suitable. Unfortunately, such models are very high dimensional and are most conveniently used when the estimation method can simultaneously perform data-driven model simplification (removal of model parameters that cannot be reliably estimated) and fitting. Such sparse reconstruction methods are typically not used in atmospheric inversions. In this work, we devise a sparse reconstruction method, and illustrate it in an idealized atmospheric inversion problem for the estimation of fossil fuel CO<sub>2</sub> (ffCO<sub>2</sub>) emissions in the lower 48 states of the USA. <br><br> Our new method is based on stagewise orthogonal matching pursuit (StOMP), a method used to reconstruct compressively sensed images. Our adaptations bestow three properties to the sparse reconstruction procedure which are useful in atmospheric inversions. We have modified StOMP to incorporate prior information on the emission field being estimated and to enforce non-negativity on the estimated field. Finally, though based on wavelets, our method allows for the estimation of fields in non-rectangular geometries, e.g., emission fields inside geographical and political boundaries. <br><br> Our idealized inversions use a recently developed multi-resolution (i.e., wavelet-based) random field model developed for ffCO<sub>2</sub> emissions and synthetic observations of ffCO<sub>2</sub> concentrations from a limited set of measurement sites. We find that our method for limiting the estimated field within an irregularly shaped region is about a factor of 10 faster than conventional approaches. It also reduces the overall computational cost by a factor of 2. Further, the sparse reconstruction scheme imposes non-negativity without introducing strong nonlinearities, such as those introduced by employing log-transformed fields, and thus reaps the benefits of simplicity and computational speed that are characteristic of linear inverse problems.http://www.geosci-model-dev.net/8/1259/2015/gmd-8-1259-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Ray
J. Lee
V. Yadav
S. Lefantzi
A. M. Michalak
B. van Bloemen Waanders
spellingShingle J. Ray
J. Lee
V. Yadav
S. Lefantzi
A. M. Michalak
B. van Bloemen Waanders
A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
Geoscientific Model Development
author_facet J. Ray
J. Lee
V. Yadav
S. Lefantzi
A. M. Michalak
B. van Bloemen Waanders
author_sort J. Ray
title A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
title_short A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
title_full A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
title_fullStr A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
title_full_unstemmed A sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
title_sort sparse reconstruction method for the estimation of multi-resolution emission fields via atmospheric inversion
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2015-04-01
description Atmospheric inversions are frequently used to estimate fluxes of atmospheric greenhouse gases (e.g., biospheric CO<sub>2</sub> flux fields) at Earth's surface. These inversions typically assume that flux departures from a prior model are spatially smoothly varying, which are then modeled using a multi-variate Gaussian. When the field being estimated is spatially rough, multi-variate Gaussian models are difficult to construct and a wavelet-based field model may be more suitable. Unfortunately, such models are very high dimensional and are most conveniently used when the estimation method can simultaneously perform data-driven model simplification (removal of model parameters that cannot be reliably estimated) and fitting. Such sparse reconstruction methods are typically not used in atmospheric inversions. In this work, we devise a sparse reconstruction method, and illustrate it in an idealized atmospheric inversion problem for the estimation of fossil fuel CO<sub>2</sub> (ffCO<sub>2</sub>) emissions in the lower 48 states of the USA. <br><br> Our new method is based on stagewise orthogonal matching pursuit (StOMP), a method used to reconstruct compressively sensed images. Our adaptations bestow three properties to the sparse reconstruction procedure which are useful in atmospheric inversions. We have modified StOMP to incorporate prior information on the emission field being estimated and to enforce non-negativity on the estimated field. Finally, though based on wavelets, our method allows for the estimation of fields in non-rectangular geometries, e.g., emission fields inside geographical and political boundaries. <br><br> Our idealized inversions use a recently developed multi-resolution (i.e., wavelet-based) random field model developed for ffCO<sub>2</sub> emissions and synthetic observations of ffCO<sub>2</sub> concentrations from a limited set of measurement sites. We find that our method for limiting the estimated field within an irregularly shaped region is about a factor of 10 faster than conventional approaches. It also reduces the overall computational cost by a factor of 2. Further, the sparse reconstruction scheme imposes non-negativity without introducing strong nonlinearities, such as those introduced by employing log-transformed fields, and thus reaps the benefits of simplicity and computational speed that are characteristic of linear inverse problems.
url http://www.geosci-model-dev.net/8/1259/2015/gmd-8-1259-2015.pdf
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