1989年3月北极地区大气CO2、CH4和CO的相关性

T.J Conway, L.P Steele , P.C Novelli
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引用次数: 36

摘要

作为第三次北极气体和气溶胶采样计划(AGASP III, 1989年3月)的一部分,在六次飞机飞行中,在整个北极对流层和平流层下层收集了189个空气样本,用于分析CO2, CH4和CO。三种气体的混合比率在水平和垂直方向上都有显着变化。在人为气溶胶浓度较高的层(北极霾)中发现浓度升高。CO2、CH4和CO的混合比在各航班上呈高度相关。对来自所有航班的汇总数据进行CH4与CO2的线性回归,得出相关系数(r2)为0.88,斜率为13.5 ppb CH4/ppm CO2 (n = 186)。对于CO vs CO2,合并线性回归得到r2 = 0.91,斜率为15.8 ppb CO/ppm CO2 (n = 182)。二氧化碳、CH4和CO的平均垂直梯度斜率分别为0.37、-4.4和- 4.2 ppb km−1。由于冬季在北极大气中观测到的二氧化碳变化主要是由于来自欧洲和亚洲的人为CO2排放和运输的变化,我们发现的强相关性表明,类似的解释适用于CH4和CO。利用对源区CO2排放的可靠估计以及测量到的CH4/CO2和CO/CO2比值,我们估计欧洲区域CH4源为47±6 Tg CH4 yr - 1,可能与化石燃料燃烧有关。对CO的类似计算结果表明,估计区域CO源为82±2 Tg CO年−1。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Correlations among atmospheric CO2, CH4 and CO in the Arctic, March 1989

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 stratosphere for analysis of CO2, CH4 and CO. The mixing ratios of the three gases varied significantly both horizontally and vertically. Elevated concentrations were found in layers with high anthropogenic aerosol concentrations (Arctic Haze). The mixing ratios of CO2, CH4 and CO were highly correlated on all flights. A linear regression of CH4 vs CO2 for pooled data from all flights yielded a correlation coefficient (r2) of 0.88 and a slope of 13.5 ppb CH4/ppm CO2 (n = 186). For CO vs CO2 a pooled linear regression gave r2 = 0.91 and a slope of 15.8 ppb CO/ppm CO2 (n = 182). Carbon dioxide, CH4 and CO also exhibited mean vertical gradients with slopes of 0.37, –4.4 and −4.2 ppb km−1, respectively.

Since the carbon dioxide variations observed in the Arctic atmosphere during winter are due primarily to variations in the emissions and transport of anthropogenic CO2 from Europe and Asia, the strong correlations that we have found suggest that a similar interpretation applies to CH4 and CO. Using reliable estimates of CO2 emissions for the source 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 associated with fossil fuel combustion. A similar calculation for CO results in an estimated regional CO source of 82±2 Tg CO yr−1.

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