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Quantifying the contributions of natural emissions to ozone and total fine PM concentrations in the Northern Hemisphere

机译:量化自然排放对北半球臭氧和总PM浓度的贡献

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pstrongAbstract./strong Accurate estimates of emissions from natural sources are needed for reliable predictions of ozone and fine particulate matter (PMsub2.5/sub) using air quality models. In this study, the large-scale atmospheric chemistry transport model, DEHM (the Danish Eulerian Hemispheric Model) is further developed, evaluated and applied to study and quantify the contributions of natural emissions of VOCs, NOsubx/sub, NHsub3/sub, SOsub2/sub, CHsub4/sub, PM, CO and sea salt to the concentration of ozone and formation of PMsub2.5/sub for the year 2006. Natural source categories adopted in the recent model are vegetation, lightning, soils, wild animals and oceans. In this study, the model has been further developed to include more Biogenic Volatile Organic Compounds (BVOCs) and to implement a scheme for secondary organic aerosols as well as an updated description of sea-salt emissions. Our simulations indicate that in the Northern Hemisphere the contribution from natural emissions to the average annual ozone mixing ratios over land is between 4a??30 ppbV. Among the natural emissions, BVOCs are found to be the most significant contributors to ozone formation in 2006, enhancing the average ozone mixing ratio by about 11% over the land areas of the Northern Hemisphere. The relative contribution of all the natural emissions to ozone is found to be highest in the northern part of South America by about 42%. Similarly, the highest contribution of all the natural sources to total fine particles over land is found to be in South America by about 74% and sea-salt aerosols demonstrated to play the most important role. However, over the rest of the regions in the model domain the largest contribution from the natural sources to PMsub2.5/sub in the specific year 2006 is due to wildfires. The contribution from natural emissions to the mean PMsub2.5/sub concentration over the land areas in the model domain is about 34%./p.
机译:> >摘要。要使用空气质量模型对臭氧和细颗粒物(PM 2.5 )进行可靠的预测,就需要准确估算自然来源的排放量。在这项研究中,进一步开发,评估和应用了大规模大气化学迁移模型DEHM(丹麦欧拉半球模型),以研究和量化VOC,NO x 的自然排放的贡献, NH 3 ,SO 2 ,CH 4 ,PM,CO和海盐对臭氧浓度和PM 2.5 < / sub>表示2006年。最近的模型采用的自然源类别为植被,闪电,土壤,野生动物和海洋。在这项研究中,该模型已得到进一步开发,以包含更多的生物挥发性有机化合物(BVOC),并实施了次级有机气溶胶方案以及对海盐排放的更新描述。我们的模拟表明,在北半球,自然排放对陆地上年平均臭氧混合比的贡献在4a?30 ppbV之间。在自然排放中,BVOC被认为是2006年臭氧形成的最主要贡献者,在北半球的陆地区域将平均臭氧混合比提高了约11%。发现所有自然排放物对臭氧的相对贡献在南美北部最高,约为42%。同样,在南美,所有自然资源对陆地上总细颗粒的贡献最大,约为74%,而海盐气溶胶显示出最重要的作用。但是,在模型域的其他区域中,自然资源在2006年特定年份对PM 2.5 的贡献最大,是由于野火。在模型域内,自然排放对陆地平均PM 2.5 浓度的贡献约为34%。

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