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Foreign and domestic contributions to springtime ozone over China

机译:对中国春天臭氧的外国和国内贡献

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China is facing a severe ozone problem, but the origin of its ozone remains unclear. Here we use a GEOS-Chem based global–regional two-way coupled model system to quantify the individual contributions of eight emission source regions worldwide to springtime ozone in 2008 over China. The model reproduces the observed ozone from 31 ground sites and various aircraft and ozonesonde measurements in China and nearby countries, with a mean bias of 10%–15% both near the surface and in the troposphere. We then combine zero-out simulations, tagged ozone simulations, and a linear weighting approach to account for the effect of nonlinear chemistry on ozone source attribution. We find considerable contributions of total foreign anthropogenic emissions to surface ozone over China (2–11ppb). For ozone of anthropogenic origin averaged over China, foreign regions together contribute 40%–60% below the height of 2km and 85% in the upper troposphere. For total ozone contributed by foreign anthropogenic emissions over China at various heights, the portion of transboundary ozone produced within foreign emission source regions is less than 50%, with the rest produced by precursors transported out of those source regions. Japan and Korea contribute 0.6–2.1ppb of surface ozone over the east coastal regions. Southeast Asia contributes 1–5ppb over much of southern China and South Asia contributes up to 5–10ppb of surface ozone over the border of southwestern China; and their contributions increase with height due to strong upwelling over the source regions. The European contribution reaches 2.1–3.0ppb for surface ozone over the northern border of China and 1.5ppb in the lower troposphere averaged over China. North America contributes 0.9–2.7ppb of surface ozone over most of China (1.5–2.1ppb over the North China Plain), with a China average at 1.5–2.5ppb at different heights below 8km, due to its large anthropogenic emissions and the transport-favorable midlatitude westerly wind. In addition to domestic emission control, global emission reduction is critical for China's ozone mitigation.
机译:中国面临着严重的臭氧问题,但臭氧的起源仍然不清楚。在这里,我们使用基于Geos-Chem基础的全球区域双向耦合模型系统来量化全球八个排放源区的各个贡献,2008年在中国汇总臭氧。该模型在中国和附近的国家和各种飞机和臭氧地区测量的观察到的臭氧再现了观察到的臭氧,在地表和对流层附近的平均偏差为10%-15%。然后,我们将零消耗模拟,标记的臭氧模拟,以及线性加权方法来解释非线性化学对臭氧源归因的影响。我们发现对中国表面臭氧的外来人为释放总体的相当大的贡献(2-11ppb)。对于在中国平均的人为原产地的臭氧,外国地区在整个对流层中贡献40%-60%以下的高度和85%。对于在各种高度的外国人为排放贡献的总臭氧,在外源区内产生的跨界臭氧部分小于50%,其剩余的前体产生从这些源区输出。日本和韩国在东沿海地区贡献了0.6-2.1ppb的表面臭氧。南亚南亚南亚贡献了1-5ppb,南亚占中国西南部边境的高达5-10ppb的表面臭氧;由于源区的强烈升值,它们的贡献随着高度而增加。欧洲贡献达到了2.1-3.0ppb,在中国北部边界和1.5ppb较低的对流层均在中国平均。北美贡献了0.9-2.7ppb的中国大部分地区臭氧(北方华北平原1.5-2.1ppb),由于其大量的人为排放和运输,以低于8km的不同高度为1.5-2.5ppb。 - 适用于中间风。除国内排放控制外,全球排放对中国臭氧缓解至关重要。

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