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Chemical transport model ozone simulations for spring 2001 over the western Pacific: Regional ozone production and its global impacts

机译:西太平洋2001年春季的化学运输模型臭氧模拟:区域臭氧生产及其全球影响

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摘要

The spatial and temporal variation in ozone production over major source regions in East Asia during the NASA Transport and Chemical Evolution over the Pacific (TRACE-P) measurement campaign in spring 2001 is assessed using a global chemical transport model. There is a strong latitudinal gradient in ozone production in springtime, driven by regional photochemistry, which rapidly diminishes as the season progresses. The great variability in meteorological conditions characteristic of East Asia in springtime leads to large daily variability in regional ozone formation, but we find that it has relatively little impact on the total global production. We note that transport processes effectively modulate and thus stabilize total ozone production through their influence over its location. However, the impact on the global ozone burden, important for assessing the effects of precursor emissions on tropospheric oxidizing capacity and climate, is sensitive to local meteorology through the effects of location on chemical lifetime. Stagnant, anticyclonic conditions conducive to substantial boundary layer ozone production typically allow little lifting of precursors into the free troposphere where greater ozone production could occur, and the consequent shorter chemical lifetime for ozone leads to relatively small impacts on global ozone. Conversely, cyclonic conditions with heavy cloud cover suppressing regional ozone production are often associated with substantial cloud convection, enhancing subsequent production in the free troposphere where chemical lifetimes are longer, and the impacts on global ozone are correspondingly greater. We find that ozone formation in the boundary layer and free troposphere outside the region of precursor emissions dominates total gross production from these sources in springtime, and that it makes a big contribution to the long range transport of ozone, which is greatest in this season.
机译:使用全球化学物运输模型评估了2001年春季NASA太平洋运输和化学演化(TRACE-P)测量活动期间东亚主要来源地区臭氧生产的时空变化。在春季,由于区域光化学的作用,臭氧产生的纬度梯度很强,随着季节的发展,臭氧的纬度迅速减少。春季东亚地区气象条件的巨大变化导致区域臭氧形成的日变化较大,但我们发现这对全球总产量的影响相对较小。我们注意到,运输过程通过对其位置的影响,有效地调节了臭氧的总产量,从而稳定了臭氧的总产量。但是,对全球臭氧负担的影响对于评估前驱物排放对流层氧化能力和气候的影响很重要,但其位置对化学物质寿命的影响对当地的气象学很敏感。停滞,反气旋的条件有利于大量边界层臭氧的产生,通常使前体几乎无法举升到可能产生更大臭氧的对流层中,因此,臭氧的化学寿命较短,对全球臭氧的影响相对较小。相反,具有浓厚云层覆盖的气旋条件会抑制区域臭氧的产生,这通常与大量的云对流有关,从而增加了化学寿命更长的自由对流层的后续生产,对全球臭氧的影响也相应更大。我们发现,在春季,在前驱物排放区域外的边界层和自由对流层中形成的臭氧占主导地位,这些来源的总总产量占主导地位,这对臭氧的远距离运输做出了巨大贡献,这是本季节中最大的。

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