Browse monthly mean maps of emissions from April 2000 to March 2001 for each source:
Click here to download numerical values for each source on a T42 grid (128 longitudes and 64 latitudes) and all 12 months. The results are saved in one netCDF file.
This page presents results of inverse modeling of surface sources of carbon monoxide with MOPITT data and global chemistry transport model MOZART 2. This research was sponsored by the MOPITT program and NASA interdisciplinary grant "A study of Tropospheric Budgets of CO and CH4 Using Data Assimilation". A final report to NASA can be found here: EOS IDS Final Report.
The overall technical goal of this study was to apply mathematical techniques of estimation theory to global atmospheric model and observational data to constrain poorly known model parameters (e.g., surface emissions of CO, OH distributions), and to improve our ability to predict the future evolution of the chemical composition of the troposphere. We employ Bayesian inversion approach for deriving surface sources of carbon monoxide from MOPITT data. Inverse modeling of surface emissions is being performed for different seasons with the goal to estimate temporal variability of the surface fluxes.
Check out this article from NASA's Earth observatory to learn more about importance of CO. Click on the left picture below to see an animation of time evotion of CO emitted from different continents. Click on the right picture to see evolution of CO emitted by 50 largest polluters in Coloradon in Dec 2001.
The direct surface emissions of CO were adjusted to minimize the disagreements between the MOPITT data and the distribution of CO computed with the MOZART 2 model. The transport model uses NCEP or ECMWF re-analysis dynamical fields. The chemical production of CO is not optimized. A priori monthly emissions are taken from an early version of EDGAR_v3 and GEIA inventories are used for the inversion.
Five sources of emissions were optimized: biomass burning, anthropogenic, biofuel, biogenic, and oceanic. Emissions for each source were derived for 12 months starting from April 2000 until March 2001.

Technical details can be found in the publications and presentations listed at the bottom of this page.
Recent presentations:
Chemical Weather Workshop, Munich 2002
CO Boulder Applied Math Colloquium March 1, 2001
Related publications:
G. Pétron, C. Granier, B. Khattatov, V. Yudin, J.-F. Lamarque, L.Emmons , J.Gille, and D. Edwards, Monthly CO surface sources inventory based on the 2000-2001 MOPITT satellite data, Geopys. Res. Lett., submitted.
Lamarque et al., Application of a bias estimator for improved assimilation of carbon monoxide MOPITT retrievals, Geophys. Res. Lett., submitted.
Pétron G., Modélisation inverse des émissions du monoxyde de carbone, THESE DE DOCTORAT DE L’UNIVERSITE PARIS 6, 10 Juillet 2003
Pétron G., et al., Inverse modeling of carbon monoxide surface emissions using NOAA-CMDL network observations, J. Geophys. Res., 107, 4761, 2002.
MOZART 2 model CO simulations were compared with independent data for validation of our results. Click here to see these comparisons.
One of the most interesting findings of this project was that CO emissions from North America and Southeast Asia have been significantly underestimated.The two plots below demonstrate this.
The derived optimized emissions were used to simulate global distribution and time evolution of carbon monoxide in the atmosphere with the MOZART 2 model. Graphics below show instantaneous 3-D iso-surfaces of simulated CO distribution superimposed on the Earth's topography. Click on the figures to see bigger plots. Or click on this link to see an animation of these results.