为 GISS ModelE2.1 地球系统模型评估丙酮

Alexandra Rivera, K. Tsigaridis, G. Faluvegi, D. Shindell
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摘要

摘要丙酮是大气中一种丰富的挥发性有机化合物(VOC),对臭氧和氧化能力有重要影响。直接来源包括其他挥发性有机化合物和人为排放物的化学生成、陆地植被、生物质燃烧排放和海洋生成。吸收汇包括化学损失、陆地表面沉积和海洋吸收。丙酮的寿命也很长,足以在远离其来源的地方与其他化合物发生迁移和反应。美国宇航局戈达德空间研究所(GISS)的地球系统模型 ModelE2.1 模拟了地球系统的各种相互作用。以前,丙酮在 ModelE 化学方案中的表示非常简单。本研究评估了一个更复杂的丙酮方案,在该方案中,丙酮是一个完整的三维示踪剂,具有明确的来源、汇和大气传输。我们首先根据过去的文献对新的全球丙酮预算进行了评估。估计的源和汇通量在以往模型的范围内,但大气总负荷和寿命在已发表文献的低端。丙酮在 ModelE2.1 中的新表现形式也使空间和垂直分布更加真实,我们将其与以前的模型和实地观测结果进行了比较。我们还结合实地测量结果对丙酮相关过程的季节性进行了研究,这些比较结果表明,在高排放的城市地区,模型的分辨率太低,无法捕捉到真实的行为,因此两者的一致性很好,但也存在不足之处。最后,我们进行了各种敏感性研究,探讨关键参数对丙酮预算及其全球分布的影响。一个有影响的发现是,前驱体碳氢化合物氧化产生的丙酮对整个化学源具有很强的杠杆作用,这表明准确的摩尔产量非常重要。总之,我们的实施与之前的研究相吻合,标志着 GISS ModelE2.1 中丙酮示踪剂的开发有了重大改进。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessing acetone for the GISS ModelE2.1 Earth system model
Abstract. Acetone is an abundant volatile organic compound (VOC) in the atmosphere, with important influences on ozone and oxidation capacity. Direct sources include chemical production from other VOCs and anthropogenic emissions, terrestrial vegetation, biomass-burning emissions, and ocean production. Sinks include chemical loss, deposition onto the land surface, and ocean uptake. Acetone also has a lifetime that is long enough to allow transport and reactions with other compounds remote from its sources. The NASA Goddard Institute for Space Studies (GISS) Earth system model ModelE2.1 simulates a variety of Earth system interactions. Previously, acetone had a very simplistic representation in the ModelE chemical scheme. This study assesses a more sophisticated acetone scheme in which acetone is a full 3-dimensional tracer with explicit sources, sinks, and atmospheric transport. We first evaluate the new global acetone budget in the context of past literature. Estimated source and sink fluxes fall within the range of previous models, although total atmospheric burden and lifetime are at the lower end of the published literature. Acetone's new representation in ModelE2.1 also results in more realistic spatial and vertical distributions, which we compare against previous models and field observations. The seasonality of acetone-related processes was also studied in conjunction with field measurements, and these comparisons show promising agreement but also shortcomings at high-emission urban locations, where the model's resolution is too coarse to capture the true behavior. Finally, we conduct a variety of sensitivity studies that explore the influence of key parameters on the acetone budget and its global distribution. An impactful finding is that the production of acetone from precursor hydrocarbon oxidation has strong leverage on the overall chemical source, indicating the importance of accurate molar yields. Overall, our implementation is one that corroborates with previous studies and marks a significant improvement in the development of the acetone tracer in GISS ModelE2.1.
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