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Atmospheric processing of iron in mineral and combustion aerosols: development of an intermediate-complexity mechanism suitable for Earth system models

机译:矿物和燃烧气溶胶中铁的大气处理:开发适用于地球系统模型的中间复杂机制

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Atmospheric processing of iron in dust and combustion aerosols is simulated using an intermediate-complexity soluble iron mechanism designed for Earth system models. The solubilization mechanism includes both a dependence on aerosol water pH and in-cloud oxalic acid. The simulations of size-resolved total, soluble and fractional iron solubility indicate that this mechanism captures many but not all of the features seen from cruise observations of labile iron. The primary objective was to determine the extent to which our solubility scheme could adequately match observations of fractional iron solubility. We define a semi-quantitative metric as the model mean at points with observations divided by the observational mean (MMO). The model is in reasonable agreement with observations of fractional iron solubility with an MMO of 0.86. Several sensitivity studies are performed to ascertain the degree of complexity needed to match observations; including the oxalic acid enhancement is necessary, while different parameterizations for calculating model oxalate concentrations are less important. The percent change in soluble iron deposition between the reference case (REF) and the simulation with acidic processing alone is 63.8?%, which is consistent with previous studies. Upon deposition to global oceans, global mean combustion iron solubility to total fractional iron solubility is 8.2?%; however, the contribution of fractional iron solubility from combustion sources to ocean basins below 15 sup°/sup S is approximately 50?%. We conclude that, in many remote ocean regions, sources of iron from combustion and dust aerosols are equally important. Our estimates of changes in deposition of soluble iron to the ocean since preindustrial climate conditions suggest roughly a doubling due to a combination of higher dust and combustion iron emissions along with more efficient atmospheric processing.
机译:使用为地球系统模型设计的中等复杂性可溶性铁机制模拟了粉尘和燃烧气溶胶中铁的大气处理。增溶机理既包括对气溶胶水pH值的依赖,也包括云中草酸的依赖。大小分辨的总铁,可溶铁和分数铁的溶解度的模拟表明,该机制捕获了从不稳定铁的巡航观测中看到的许多但不是全部特征。主要目的是确定我们的溶解度方案在何种程度上可以充分匹配分数铁溶解度的观察结果。我们将半定量度量定义为观测点除以观测均值(MMO)的模型均值。该模型与铁的分数溶解度(MMO为0.86)的观察结果合理一致。进行了几项敏感性研究,以确定匹配观察结果所需的复杂程度;包括草酸增强剂是必需的,而用于计算模型草酸浓度的不同参数设置则不太重要。在参考案例(REF)和仅使用酸性工艺进行的模拟之间,可溶性铁沉积的变化百分比为63.8%,与先前的研究一致。沉积到全球海洋中后,全球平均燃烧铁溶解度相对于总铁溶解度为8.2%。但是,从燃烧源到低于15 ° S的海洋盆地的铁溶解度分数贡献约为50%。我们得出结论,在许多偏远的海洋地区,来自燃烧和粉尘气溶胶的铁源同样重要。自工业化前的气候条件以来,我们对可溶性铁在海洋中沉积变化的估计表明,由于较高的粉尘和燃烧铁的排放量以及更有效的大气处理过程,使可溶性铁的含量大致翻了一番。

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