Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget

Most previous top-down global carbon monoxide (CO) budget estimates have used only concentration information and shown large differences in individual source estimates. Since CO from certain sources has a specific isotopic signature, coupling the concentration and isotope fraction information can pr...

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Main Authors: Keyhong Park, Louisa K. Emmons, Zhihui Wang, John E. Mak
Format: Article
Language:English
Published: MDPI AG 2015-04-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/6/5/547
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author Keyhong Park
Louisa K. Emmons
Zhihui Wang
John E. Mak
author_facet Keyhong Park
Louisa K. Emmons
Zhihui Wang
John E. Mak
author_sort Keyhong Park
collection DOAJ
description Most previous top-down global carbon monoxide (CO) budget estimates have used only concentration information and shown large differences in individual source estimates. Since CO from certain sources has a specific isotopic signature, coupling the concentration and isotope fraction information can provide a better constraint on CO source strength estimates. We simulate both CO concentration and its oxygen isotopologue C18O in the 3-D global chemical transport model MOZART-4 and compare the results with observations. We then used a Bayesian inversion to calculate the most probable global CO budget. In the analysis, δ18O information is jointly applied with concentration. The joint inversion results should provide more accurate and precise inversion results in comparison with CO-only inversion. Various methods combining the concentration and isotope ratios were tested to maximize the benefit of including isotope information. The joint inversion of CO and δ18O estimated total global CO production at 2951 Tg-CO/yr in 1997, 3084 Tg-CO/yr in 1998, and 2583 Tg-CO/yr in 2004. The updated CO budget improved both the modeled CO and δ18O. The clear improvement shown in the δ18O implies that more accurate source strengths are estimated. Thus, we confirmed that the observation of CO isotopes provide further substantial information for estimating a global CO budget.
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spelling doaj.art-5670717d8e8041a5bb7149f3fabb1f162022-12-21T19:41:24ZengMDPI AGAtmosphere2073-44332015-04-016554757810.3390/atmos6050547atmos6050547Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO BudgetKeyhong Park0Louisa K. Emmons1Zhihui Wang2John E. Mak3Institute for Terrestrial and Planetary Atmospheres, School of Marine and Atmospheric Sciences, State University of New York at Stony Brook, Stony Brook, NY 11794, USAAtmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO 80301, USAInstitute for Terrestrial and Planetary Atmospheres, School of Marine and Atmospheric Sciences, State University of New York at Stony Brook, Stony Brook, NY 11794, USAInstitute for Terrestrial and Planetary Atmospheres, School of Marine and Atmospheric Sciences, State University of New York at Stony Brook, Stony Brook, NY 11794, USAMost previous top-down global carbon monoxide (CO) budget estimates have used only concentration information and shown large differences in individual source estimates. Since CO from certain sources has a specific isotopic signature, coupling the concentration and isotope fraction information can provide a better constraint on CO source strength estimates. We simulate both CO concentration and its oxygen isotopologue C18O in the 3-D global chemical transport model MOZART-4 and compare the results with observations. We then used a Bayesian inversion to calculate the most probable global CO budget. In the analysis, δ18O information is jointly applied with concentration. The joint inversion results should provide more accurate and precise inversion results in comparison with CO-only inversion. Various methods combining the concentration and isotope ratios were tested to maximize the benefit of including isotope information. The joint inversion of CO and δ18O estimated total global CO production at 2951 Tg-CO/yr in 1997, 3084 Tg-CO/yr in 1998, and 2583 Tg-CO/yr in 2004. The updated CO budget improved both the modeled CO and δ18O. The clear improvement shown in the δ18O implies that more accurate source strengths are estimated. Thus, we confirmed that the observation of CO isotopes provide further substantial information for estimating a global CO budget.http://www.mdpi.com/2073-4433/6/5/547carbon monoxideinverse modelingisotopeglobal CO budget
spellingShingle Keyhong Park
Louisa K. Emmons
Zhihui Wang
John E. Mak
Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
Atmosphere
carbon monoxide
inverse modeling
isotope
global CO budget
title Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
title_full Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
title_fullStr Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
title_full_unstemmed Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
title_short Joint Application of Concentration and δ18O to Investigate the Global Atmospheric CO Budget
title_sort joint application of concentration and δ18o to investigate the global atmospheric co budget
topic carbon monoxide
inverse modeling
isotope
global CO budget
url http://www.mdpi.com/2073-4433/6/5/547
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AT louisakemmons jointapplicationofconcentrationandd18otoinvestigatetheglobalatmosphericcobudget
AT zhihuiwang jointapplicationofconcentrationandd18otoinvestigatetheglobalatmosphericcobudget
AT johnemak jointapplicationofconcentrationandd18otoinvestigatetheglobalatmosphericcobudget