4.6 Article

Monitoring carbon dioxide from space: Retrieval algorithm and flux inversion based on GOSAT data and using CarbonTracker-China

Journal

ADVANCES IN ATMOSPHERIC SCIENCES
Volume 34, Issue 8, Pages 965-976

Publisher

SCIENCE PRESS
DOI: 10.1007/s00376-017-6221-4

Keywords

retrieval algorithm; satellite remote sensing; CO2; carbon flux; GOSAT

Funding

  1. Strategic Priority Research Program-Climate Change: Carbon Budget and Relevant Issues [XDA05040200]
  2. National Key Research and Development Program of China [2016YFA0600203]
  3. National Natural Science Foundation of China [41375035, 31500402]
  4. Chinese Academy of Sciences Strategic Priority Program on Space Science [XDA04077300]

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Monitoring atmospheric carbon dioxide (CO2) from space-borne state-of-the-art hyperspectral instruments can provide a high precision global dataset to improve carbon flux estimation and reduce the uncertainty of climate projection. Here, we introduce a carbon flux inversion system for estimating carbon flux with satellite measurements under the support of The Strategic Priority Research Program of the Chinese Academy of Sciences-Climate Change: Carbon Budget and Relevant Issues. The carbon flux inversion system is composed of two separate parts: the Institute of Atmospheric Physics Carbon Dioxide Retrieval Algorithm for Satellite Remote Sensing (IAPCAS), and CarbonTracker-China (CT-China), developed at the Chinese Academy of Sciences. The Greenhouse gases Observing SATellite (GOSAT) measurements are used in the carbon flux inversion experiment. To improve the quality of the IAPCAS-GOSAT retrieval, we have developed a post-screening and bias correction method, resulting in 25%-30% of the data remaining after quality control. Based on these data, the seasonal variation of XCO2 (column-averaged CO2 dry-air mole fraction) is studied, and a strong relation with vegetation cover and population is identified. Then, the IAPCAS-GOSAT XCO2 product is used in carbon flux estimation by CT-China. The net ecosystem CO2 exchange is -0.34 Pg C yr(-1) (+/- 0.08 Pg C yr(-1)), with a large error reduction of 84%, which is a significant improvement on the error reduction when compared with in situ-only inversion.

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