Atmospheric Science
Global CO2 distributions over land from the Greenhouse Gases Observing Satellite (GOSAT)
Article first published online: 21 APR 2012
DOI: 10.1029/2012GL051203
Copyright 2012 by the American Geophysical Union
Additional Information
How to Cite
, , , and (2012), Global CO2 distributions over land from the Greenhouse Gases Observing Satellite (GOSAT), Geophys. Res. Lett., 39, L08804, doi:10.1029/2012GL051203.
Publication History
- Issue published online: 21 APR 2012
- Article first published online: 21 APR 2012
- Manuscript Accepted: 22 MAR 2012
- Manuscript Revised: 15 MAR 2012
- Manuscript Received: 2 FEB 2012
Funded by
- National Aeronautics and Space Administration (NASA). Grant Number: NNX08AJ92G
Keywords:
- GOSAT carbon dioxide;
- data-driven Level 3 products;
- global mapping;
- high-resolution;
- model intercomparison;
- uncertainty quantification
[1] January 2009 saw the successful launch of the first space-based mission specifically designed for measuring greenhouse gases, the Japanese Greenhouse gases Observing SATellite (GOSAT). We present global land maps (Level 3 data) of column-averaged CO2 concentrations (XCO2) derived using observations from the GOSAT ACOS retrieval algorithm, for July through December 2009. The applied geostatistical mapping approach makes it possible to generate maps at high spatial and temporal resolutions that include uncertainty measures and that are derived directly from the Level 2 observations, without invoking an atmospheric transport model or estimates of CO2uptake and emissions. As such, they are particularly well suited for comparison studies. Results show that the Level 3 maps for July to December 2009 on a 1° × 1.25° grid, at six-day resolution capture much of the synoptic scale and regional variability of XCO2, in addition to its overall seasonality. The uncertainty estimates, which reflect local data coverage, XCO2variability, and retrieval errors, indicate that the Southern latitudes are relatively well-constrained, while the Sahara Desert and the high Northern latitudes are weakly-constrained. A probabilistic comparison to the PCTM/GEOS-5/CASA-GFED model reveals that the most statistically significant discrepancies occur in South America in July and August, and central Asia in September to December. While still preliminary, these results illustrate the usefulness of a high spatiotemporal resolution, data-driven Level 3 data product for direct interpretation and comparison of satellite observations of highly dynamic parameters such as atmospheric CO2.

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