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A preliminary three-dimensional global model study of atmospheric methyl chloride distributions

机译:大气甲基氯分布的初步三维全球模型研究

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摘要

A global three-dimensional atmospheric model of methyl chloride (CH3Cl) is presented. When incorporating known terrestrial and oceanic source terms, the tropospheric budget of CH3Cl is unbalanced. We show that a reduction in the atmospheric CH3Cl loss rate could account for the net budget discrepancy but fails to reproduce the observed latitudinal distribution. We rind that observed mixing ratios and latitudinal distributions can be reproduced by addition of a tropical terrestrial CH3Cl source of 2330-2430 Gg yr(-1) combined with a 50% reduction in the southeastern Asian biomass burning contribution. This is equivalent to a net source of 3800-3900 Gg yr(-1), slightly higher than previously estimated. The magnitude of additional emissions required to match observations is sensitive to their latitudinal distribution. We successfully simulate tropical land-bascd observations best when the added source is increased at the coasts relative to inland areas. Mixing ratios at remote sites are relatively insensitive to the finer details of the source parameterization.
机译:提出了一个全球三维三维大气模型的氯甲烷(CH3Cl)。当结合已知的陆源和海洋源项时,CH3Cl的对流层预算不平衡。我们表明,大气中CH3Cl损失率的降低可以解释净预算差异,但无法重现观察到的纬度分布。我们磨碎了观察到的混合比和纬度分布可以通过添加2330-2430 Gg yr(-1)的热带陆地CH3Cl源以及东南亚生物质燃烧贡献降低50%的方式来再现。这相当于3800-3900 Gg yr(-1)的净源,略高于先前的估计。匹配观测值所需的额外排放量对其纬度分布很敏感。当相对于内陆地区的沿海地区增加的源增加时,我们可以最好地成功模拟热带陆基观测。远程站点的混合比例对源参数化的详细信息相对不敏感。

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