4.7 Article

Temporal changes in the emissions of CH4 and CO from China estimated from CH4/CO2 and CO/CO2 correlations observed at Hateruma Island

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ATMOSPHERIC CHEMISTRY AND PHYSICS
卷 14, 期 3, 页码 1663-1677

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COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-14-1663-2014

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  1. Grants-in-Aid for Scientific Research [24710003] Funding Source: KAKEN

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In situ observation of the atmospheric CO2, CH4, and CO mixing ratios at Hateruma Island (HAT, 24.05 degrees N, 123.80 degrees E) often show synoptic-scale variations with correlative elevations during winter, associated with air transport from the East Asian countries. We examine winter (November-March) trends in Delta CH4 / Delta CO2, Delta CO/ Delta CO2, and Delta CO/ Delta CH4 observed at Hateruma over the period 1999 to 2010. To investigate the relationship between the East Asian emissions and the short-term variations in the atmospheric mixing ratios, we use the FLEXPART Lagrangian particle dispersion model (LPDM). The observed ratios Delta CH4 / Delta CO2 and Delta CO/ Delta CO2 both show an overall gradual decrease over the study period due to a recent rapid increase in fossil fuel consumption in China. We note, however, that the decreasing rates of Delta CH4 / Delta CO2 and Delta CO/ Delta CO2 show gradual decrease and increase, respectively, during the entire observation periods used in this study. The Delta CO/ Delta CH4 slope, on the other hand, shows an increasing trend during 1999-2004 but a decrease during 2005-2010. Calculation of the concentration footprint for the atmospheric observation at HAT by using the FLEXPART LPDM indicates that most of the short-term variations are caused by emission variations from northern and eastern China. Combined with a set of reported emission maps, we have estimated the temporal changes in the annual CH4 and CO emissions from China under the assumption that the estimate of the fossil-fuel-derived CO2 emissions based on the energy statistics are accurate. The estimated annual CH4 emissions, corresponding to nonseasonal sources or anthropogenic sources without rice fields, show a nearly constant value of 39 +/- 7 TgCH(4) yr(-1) during 1998-2002, and then gradually increase to 46 +/- 8 TgCH(4) yr(-1) in 2009/2010. The estimated annual CO emissions increase from 134 +/- 32 TgCO yr(-1) in 1998/1999 to 182 +/- 42 TgCO yr(-1) in 2004/2005, level off after 2005, and then slightly decrease to less than 160 TgCO yr(-1) in 2008-2010.

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