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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Bibliographic Details
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