Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites
Atmospheric column-averaged mole fractions of carbon dioxide (XCO<sub>2</sub>) at 53 locations around the world were derived from aircraft measurements covering the altitude range of about 1–10 km. We used CO<sub>2</sub> vertical profile measurements from three major carbon c...
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Series: | Atmospheric Chemistry and Physics |
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doaj-7867313bb10c40b4b07799c7a507b8472020-11-25T00:41:52ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-05-0113105265527510.5194/acp-13-5265-2013Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sitesY. MiyamotoM. InoueI. MorinoO. UchinoT. YokotaT. MachidaY. SawaH. MatsuedaC. SweeneyP. P. TansA. E. AndrewsP. K. PatraAtmospheric column-averaged mole fractions of carbon dioxide (XCO<sub>2</sub>) at 53 locations around the world were derived from aircraft measurements covering the altitude range of about 1–10 km. We used CO<sub>2</sub> vertical profile measurements from three major carbon cycle programs, a global climatological data set of air number density profiles and tropopause height for calculating XCO<sub>2</sub> for the period of 2007–2009. Vertical profiles of the CO<sub>2</sub> mixing ratio are complemented by tall tower data up to 400 m from the earth's surface and by simulated profiles in the stratosphere from a chemistry-transport model. The amplitude of the seasonal cycle of calculated XCO<sub>2</sub> values shows clear latitudinal dependence, and the amplitude decreases from about 10 ppm at high latitudes in the Northern Hemisphere to at most 2 ppm in the tropics and the Southern Hemisphere. The uncertainties of XCO<sub>2</sub> were estimated from assumptions about CO<sub>2</sub> profiles for each flight. Typically, uncertainties were less than 1 ppm; thus, this data set is within the level of uncertainty needed for primary validation of XCO<sub>2</sub> measurements by the Greenhouse gases Observing SATellite (GOSAT) and by future satellite missions for monitoring greenhouse gases.http://www.atmos-chem-phys.net/13/5265/2013/acp-13-5265-2013.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Y. Miyamoto M. Inoue I. Morino O. Uchino T. Yokota T. Machida Y. Sawa H. Matsueda C. Sweeney P. P. Tans A. E. Andrews P. K. Patra |
spellingShingle |
Y. Miyamoto M. Inoue I. Morino O. Uchino T. Yokota T. Machida Y. Sawa H. Matsueda C. Sweeney P. P. Tans A. E. Andrews P. K. Patra Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites Atmospheric Chemistry and Physics |
author_facet |
Y. Miyamoto M. Inoue I. Morino O. Uchino T. Yokota T. Machida Y. Sawa H. Matsueda C. Sweeney P. P. Tans A. E. Andrews P. K. Patra |
author_sort |
Y. Miyamoto |
title |
Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
title_short |
Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
title_full |
Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
title_fullStr |
Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
title_full_unstemmed |
Atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
title_sort |
atmospheric column-averaged mole fractions of carbon dioxide at 53 aircraft measurement sites |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2013-05-01 |
description |
Atmospheric column-averaged mole fractions of carbon dioxide (XCO<sub>2</sub>) at 53 locations around the world were derived from aircraft measurements covering the altitude range of about 1–10 km. We used CO<sub>2</sub> vertical profile measurements from three major carbon cycle programs, a global climatological data set of air number density profiles and tropopause height for calculating XCO<sub>2</sub> for the period of 2007–2009. Vertical profiles of the CO<sub>2</sub> mixing ratio are complemented by tall tower data up to 400 m from the earth's surface and by simulated profiles in the stratosphere from a chemistry-transport model. The amplitude of the seasonal cycle of calculated XCO<sub>2</sub> values shows clear latitudinal dependence, and the amplitude decreases from about 10 ppm at high latitudes in the Northern Hemisphere to at most 2 ppm in the tropics and the Southern Hemisphere. The uncertainties of XCO<sub>2</sub> were estimated from assumptions about CO<sub>2</sub> profiles for each flight. Typically, uncertainties were less than 1 ppm; thus, this data set is within the level of uncertainty needed for primary validation of XCO<sub>2</sub> measurements by the Greenhouse gases Observing SATellite (GOSAT) and by future satellite missions for monitoring greenhouse gases. |
url |
http://www.atmos-chem-phys.net/13/5265/2013/acp-13-5265-2013.pdf |
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