CORRELATIONS AMONG ATMOSPHERIC CO2, CH4 AND CO IN THE ARCTIC, MARCH 1989

Citation
Tj. Conway et al., CORRELATIONS AMONG ATMOSPHERIC CO2, CH4 AND CO IN THE ARCTIC, MARCH 1989, Atmospheric environment. Part A, General topics, 27(17-18), 1993, pp. 2881-2894
Citations number
31
Categorie Soggetti
Environmental Sciences","Metereology & Atmospheric Sciences
ISSN journal
09601686
Volume
27
Issue
17-18
Year of publication
1993
Pages
2881 - 2894
Database
ISI
SICI code
0960-1686(1993)27:17-18<2881:CAACCA>2.0.ZU;2-8
Abstract
During six aircraft flights conducted as part of the third Arctic Gas and Aerosol Sampling Program (AGASP III, March 1989), 189 air samples were collected throughout the Arctic troposphere and lower stratospher e for analysis of CO2, CH4 and CO. The mixing ratios of the three gase s varied significantly both horizontally and vertically. Elevated conc entrations were found in layers with high anthropogenic aerosol concen trations (Arctic Haze), The mixing ratios of CO2, CH4 and CO were high ly correlated on all flights. A linear regression of CH4 vs CO2 for po oled data from all flights yielded a correlation coefficient (r(2)) of 0.88 and a slope of 13.5 ppb CH4/ppm CO2 (n = 186). For CO vs CO2 a p ooled linear regression gave r(2) = 0.91 and a slope of 15.8 ppb CO/pp m CO2 (n = 182). Carbon dioxide, CH4 and CO also exhibited mean vertic al gradients with slopes of 0.37, -4.4 and -4.2 ppb km(-1), respective ly. Since the carbon dioxide variations observed in the Arctic atmosph ere during winter are due primarily to variations in the emissions and transport of anthropogenic CO2 from Europe and Asia, the strong corre lations that we have found suggest that a similar interpretation appli es to CH4 and CO. Using reliable estimates of CO2 emissions for the so urce regions and the measured CH4/CO2 and CO/CO2 ratios, we estimate a regional European CH4 source of 47+/-6 Tg CH4 yr(-1) that may be asso ciated with fossil fuel combustion. A similar calculation for CO resul ts in an estimated regional CO source of 82+/- 2Tg CO yr(-1).