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...
Main Authors: | , , , , , |
---|---|
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 |
id |
doaj-22ddc369a4374e33ba1b082039a1a26c |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT jray asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT jlee asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT vyadav asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT slefantzi asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT ammichalak asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT bvanbloemenwaanders asparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT jray sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT jlee sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT vyadav sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT slefantzi sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT ammichalak sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion AT bvanbloemenwaanders sparsereconstructionmethodfortheestimationofmultiresolutionemissionfieldsviaatmosphericinversion |
_version_ |
1725482376121810944 |