Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011

In situ measurements of carbon monoxide (CO) and ozone (O<sub>3</sub>) at the Pico Mountain Observatory (PMO) located in the Azores, Portugal, are analyzed together with results from an atmospheric chemical transport model (GEOS-Chem) and satellite remote sensing data (AIRS (Atmospheric...

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Main Authors: A. Kumar, S. Wu, M. F. Weise, R. Honrath, R. C. Owen, D. Helmig, L. Kramer, M. Val Martin, Q. Li
Format: Article
Language:English
Published: Copernicus Publications 2013-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/12537/2013/acp-13-12537-2013.pdf
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author A. Kumar
S. Wu
M. F. Weise
R. Honrath
R. C. Owen
D. Helmig
L. Kramer
M. Val Martin
Q. Li
author_facet A. Kumar
S. Wu
M. F. Weise
R. Honrath
R. C. Owen
D. Helmig
L. Kramer
M. Val Martin
Q. Li
author_sort A. Kumar
collection DOAJ
description In situ measurements of carbon monoxide (CO) and ozone (O<sub>3</sub>) at the Pico Mountain Observatory (PMO) located in the Azores, Portugal, are analyzed together with results from an atmospheric chemical transport model (GEOS-Chem) and satellite remote sensing data (AIRS (Atmospheric Infrared Sounder) for CO, and TES (Tropospheric Emission Spectrometer) for O<sub>3</sub>) to examine the evolution of free-troposphere CO and O<sub>3</sub> over the North Atlantic for 2001–2011. GEOS-Chem captured the seasonal cycles for CO and O<sub>3</sub> well but significantly underestimated the mixing ratios of CO, particularly in spring. Statistically significant (using a significance level of 0.05) decreasing trends were found for both CO and O<sub>3</sub> based on harmonic regression analysis of the measurement data. The best estimates of the possible trends for CO and O<sub>3</sub> measurements are −0.31 ± 0.30 (2-σ) ppbv yr<sup>−1</sup> and −0.21 ± 0.11 (2-σ) ppbv yr<sup>−1</sup>, respectively. Similar decreasing trends for both species were obtained with GEOS-Chem simulation results. The most important factor contributing to the decreases in CO and O<sub>3</sub> at PMO over the past decade is the decline in anthropogenic emissions from North America, which more than compensate for the impacts from increasing Asian emissions. It is likely that climate change in the past decade has also affected the intercontinental transport of O<sub>3</sub>.
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spelling doaj.art-f1e0071a53b24141bdc97ab2698d219a2022-12-22T01:25:27ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-12-011324125371254710.5194/acp-13-12537-2013Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011A. Kumar0S. Wu1M. F. Weise2R. Honrath3R. C. Owen4D. Helmig5L. Kramer6M. Val Martin7Q. Li8Department of Civil & Environmental Engineering, Michigan Technological University, Houghton, Michigan, USADepartment of Civil & Environmental Engineering, Michigan Technological University, Houghton, Michigan, USADepartment of Civil & Environmental Engineering, Michigan Technological University, Houghton, Michigan, USADepartment of Civil & Environmental Engineering, Michigan Technological University, Houghton, Michigan, USAUS EPA, Research Triangle Park, North Carolina, USAInstitute of Alpine and Arctic Research, University of Colorado at Boulder, Boulder, Colorado, USADepartment of Geological and Mining Engineering and Sciences, Michigan Technological University, Houghton, Michigan, USADepartment of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado, USADepartment of Atmospheric {&} Oceanic Sciences, University of California Los Angeles, Los Angeles, California, USAIn situ measurements of carbon monoxide (CO) and ozone (O<sub>3</sub>) at the Pico Mountain Observatory (PMO) located in the Azores, Portugal, are analyzed together with results from an atmospheric chemical transport model (GEOS-Chem) and satellite remote sensing data (AIRS (Atmospheric Infrared Sounder) for CO, and TES (Tropospheric Emission Spectrometer) for O<sub>3</sub>) to examine the evolution of free-troposphere CO and O<sub>3</sub> over the North Atlantic for 2001–2011. GEOS-Chem captured the seasonal cycles for CO and O<sub>3</sub> well but significantly underestimated the mixing ratios of CO, particularly in spring. Statistically significant (using a significance level of 0.05) decreasing trends were found for both CO and O<sub>3</sub> based on harmonic regression analysis of the measurement data. The best estimates of the possible trends for CO and O<sub>3</sub> measurements are −0.31 ± 0.30 (2-σ) ppbv yr<sup>−1</sup> and −0.21 ± 0.11 (2-σ) ppbv yr<sup>−1</sup>, respectively. Similar decreasing trends for both species were obtained with GEOS-Chem simulation results. The most important factor contributing to the decreases in CO and O<sub>3</sub> at PMO over the past decade is the decline in anthropogenic emissions from North America, which more than compensate for the impacts from increasing Asian emissions. It is likely that climate change in the past decade has also affected the intercontinental transport of O<sub>3</sub>.http://www.atmos-chem-phys.net/13/12537/2013/acp-13-12537-2013.pdf
spellingShingle A. Kumar
S. Wu
M. F. Weise
R. Honrath
R. C. Owen
D. Helmig
L. Kramer
M. Val Martin
Q. Li
Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
Atmospheric Chemistry and Physics
title Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
title_full Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
title_fullStr Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
title_full_unstemmed Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
title_short Free-troposphere ozone and carbon monoxide over the North Atlantic for 2001–2011
title_sort free troposphere ozone and carbon monoxide over the north atlantic for 2001 2011
url http://www.atmos-chem-phys.net/13/12537/2013/acp-13-12537-2013.pdf
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