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首页> 外文期刊>Atmospheric chemistry and physics >Temporal changes in the emissions of CH_4 and CO from China estimated from CH_4 /CO_2 and CO/CO_2 correlations observed at Hateruma Island
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Temporal changes in the emissions of CH_4 and CO from China estimated from CH_4 /CO_2 and CO/CO_2 correlations observed at Hateruma Island

机译:根据在Hateruma岛观测到的CH_4 / CO_2和CO / CO_2相关性估算的中国CH_4和CO排放的时间变化

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In situ observation of the atmospheric CO_2, CH_4, and CO mixing ratios at Hateruma Island (HAT, 24.05oN, 123.80oE) 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 ?CH_4 /?CO_2, ?CO/?CO_2, and?CO/?CH_4 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 ?CH_4 /?CO_2 and ?CO/?CO_2 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 ?CH_4 /?CO_2 and ?CO/?CO_2 show gradual decrease and increase, respectively, during the entire observation periods used in this study. The ?CO/?CH_4 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 CH_4 and CO emissions from China under the assumption that the estimate of the fossil-fuel-derived CO_2 emissions based on the energy statistics are accurate. The estimated annual CH_4 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.
机译:在Hateruma岛(HAT,24.05oN,123.80oE)对大气中CO_2,CH_4和CO混合比的原位观测通常显示天气尺度尺度的变化,并伴随冬季相关海拔的升高,与东亚国家的航空运输有关。我们研究了1999-2010年在Hateruma观测到的冬季(11月至3月)?CH_4 /?CO_2,?CO /?CO_2和?CO /?CH_4的趋势。调查了东亚排放与短期排放之间的关系。大气混合比的长期变化,我们使用FLEXPART拉格朗日粒子分散模型(LPDM)。由于近期中国化石燃料消费的快速增长,观测到的比率?CH_4 /?CO_2和?CO /?CO_2均在研究期内总体呈逐渐下降的趋势,但我们注意到?CH_4 /的下降率在本研究中使用的整个观察期内,?CO_2和?CO /?CO_2分别显示逐渐减小和增加。另一方面,?CO /?CH_4斜率在1999-2004年期间呈上升趋势,而在2005-2010年期间呈下降趋势。使用FLEXPART LPDM计算HAT大气观测的浓度足迹表明,大部分短期变化是由中国北方和东部的排放变化引起的。结合一组报告的排放图,我们假设基于能源统计数据的化石燃料衍生的CO_2排放量的估算是准确的,从而估算了中国每年CH_4和CO排放量的时间变化。在1998-2002年期间,估计的CH_4年排放量对应于非季节源或无稻田的人为源,显示39±7 TgCH_4 yr〜(-1)的近似恒定值,然后逐渐增加到46±8 TgCH_4 yr〜( -1)在2009/2010年。估计每年的CO排放量从1998/1999年的134±32 TgCO yr〜(-1)增加到2004/2005年的182±42 TgCO yr〜(-1),在2005年后趋于稳定,然后略微降低至160以下TgCO yr〜(-1)在2008-2010年。

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