Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses
The net surface exchange of CO<sub>2</sub> for the years 2002–2007 is inferred from 12 181 atmospheric CO<sub>2</sub> concentration data with a time-dependent Bayesian synthesis inversion scheme. Monthly CO<sub>2</sub> fluxes are optimized for 30 regions of the No...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2011-11-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/8/3263/2011/bg-8-3263-2011.pdf |
| _version_ | 1818877130445946880 |
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| author | J. M. Chen F. Deng |
| author_facet | J. M. Chen F. Deng |
| author_sort | J. M. Chen |
| collection | DOAJ |
| description | The net surface exchange of CO<sub>2</sub> for the years 2002–2007 is inferred from 12 181 atmospheric CO<sub>2</sub> concentration data with a time-dependent Bayesian synthesis inversion scheme. Monthly CO<sub>2</sub> fluxes are optimized for 30 regions of the North America and 20 regions for the rest of the globe. Although there have been many previous multiyear inversion studies, the reliability of atmospheric inversion techniques has not yet been systematically evaluated for quantifying regional interannual variability in the carbon cycle. In this study, the global interannual variability of the CO<sub>2</sub> flux is found to be dominated by terrestrial ecosystems, particularly by tropical land, and the variations of regional terrestrial carbon fluxes are closely related to climate variations. These interannual variations are mostly caused by abnormal meteorological conditions in a few months in the year or part of a growing season and cannot be well represented using annual means, suggesting that we should pay attention to finer temporal climate variations in ecosystem modeling. We find that, excluding fossil fuel and biomass burning emissions, terrestrial ecosystems and oceans absorb an average of 3.63 ± 0.49 and 1.94 ± 0.41 Pg C yr<sup>−1</sup>, respectively. The terrestrial uptake is mainly in northern land while the tropical and southern lands contribute 0.62 ± 0.47, and 0.67 ± 0.34 Pg C yr<sup>−1</sup> to the sink, respectively. In North America, terrestrial ecosystems absorb 0.89 ± 0.18 Pg C yr<sup>−1</sup> on average with a strong flux density found in the south-east of the continent. |
| first_indexed | 2024-12-19T13:53:23Z |
| format | Article |
| id | doaj.art-5748118287564d85bb309dc11781d38e |
| institution | Directory Open Access Journal |
| issn | 1726-4170 1726-4189 |
| language | English |
| last_indexed | 2024-12-19T13:53:23Z |
| publishDate | 2011-11-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Biogeosciences |
| spelling | doaj.art-5748118287564d85bb309dc11781d38e2022-12-21T20:18:39ZengCopernicus PublicationsBiogeosciences1726-41701726-41892011-11-018113263328110.5194/bg-8-3263-2011Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analysesJ. M. ChenF. DengThe net surface exchange of CO<sub>2</sub> for the years 2002–2007 is inferred from 12 181 atmospheric CO<sub>2</sub> concentration data with a time-dependent Bayesian synthesis inversion scheme. Monthly CO<sub>2</sub> fluxes are optimized for 30 regions of the North America and 20 regions for the rest of the globe. Although there have been many previous multiyear inversion studies, the reliability of atmospheric inversion techniques has not yet been systematically evaluated for quantifying regional interannual variability in the carbon cycle. In this study, the global interannual variability of the CO<sub>2</sub> flux is found to be dominated by terrestrial ecosystems, particularly by tropical land, and the variations of regional terrestrial carbon fluxes are closely related to climate variations. These interannual variations are mostly caused by abnormal meteorological conditions in a few months in the year or part of a growing season and cannot be well represented using annual means, suggesting that we should pay attention to finer temporal climate variations in ecosystem modeling. We find that, excluding fossil fuel and biomass burning emissions, terrestrial ecosystems and oceans absorb an average of 3.63 ± 0.49 and 1.94 ± 0.41 Pg C yr<sup>−1</sup>, respectively. The terrestrial uptake is mainly in northern land while the tropical and southern lands contribute 0.62 ± 0.47, and 0.67 ± 0.34 Pg C yr<sup>−1</sup> to the sink, respectively. In North America, terrestrial ecosystems absorb 0.89 ± 0.18 Pg C yr<sup>−1</sup> on average with a strong flux density found in the south-east of the continent.http://www.biogeosciences.net/8/3263/2011/bg-8-3263-2011.pdf |
| spellingShingle | J. M. Chen F. Deng Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses Biogeosciences |
| title | Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses |
| title_full | Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses |
| title_fullStr | Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses |
| title_full_unstemmed | Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses |
| title_short | Recent global CO<sub>2</sub> flux inferred from atmospheric CO<sub>2</sub> observations and its regional analyses |
| title_sort | recent global co sub 2 sub flux inferred from atmospheric co sub 2 sub observations and its regional analyses |
| url | http://www.biogeosciences.net/8/3263/2011/bg-8-3263-2011.pdf |
| work_keys_str_mv | AT jmchen recentglobalcosub2subfluxinferredfromatmosphericcosub2subobservationsanditsregionalanalyses AT fdeng recentglobalcosub2subfluxinferredfromatmosphericcosub2subobservationsanditsregionalanalyses |