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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Main Authors: 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
Format: Article
Language:English
Published: Copernicus Publications 2013-05-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/5265/2013/acp-13-5265-2013.pdf
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spelling 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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