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Results of an interactively coupled atmospheric chemistry – general circulation model: Comparison with observations

机译:相互作用耦合的大气化学结果–普通环流模型:与观测值的比较

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The coupledclimate-chemistry model ECHAM4.L39(DLR)/CHEM is presented which enables asimultaneous treatment of meteorology and atmospheric chemistry and theirfeedbacks. This is the first model which interactively combines a generalcirculation model with a chemical model, employing most of the importantreactions and species necessary to describe the stratospheric and uppertropospheric ozone chemistry, and which is computationally fast enough to allowlong-term integrations with currently available computer resources. This ispossible as the model time-step used for the chemistry can be chosen as large asthe integration time-step for the dynamics. Vertically the atmosphere isdiscretized by 39 levels from the surface up to the top layer which is centred at 10 hPa, with a relatively high vertical resolution of approximately 700 mnear the extra-tropical tropopause. We present the results of a controlsimulation representing recent conditions (1990) and compare it to availableobservations. The focus is on investigations of stratospheric dynamics andchemistry relevant to describe the stratospheric ozone layer. ECHAM4.L39(DLR)/CHEMreproduces main features of stratospheric dynamics in the arctic vortex region,including stratospheric warming events. This constitutes a major improvementcompared to earlier model versions. However, apparent shortcomings in Antarctic circulation and temperatures persist. The seasonal and interannual variabilityof the ozone layer is simulated in accordance with observations. Activation anddeactivation of chlorine in the polar stratospheric vortices and theirinter-hemispheric differences are reproduced. Considering methane oxidation aspart of the dynamic-chemistry feedback results in an improved representation ofthe spatial distribution of stratospheric water vapour concentrations. Thecurrent model constitutes a powerful tool to investigate, for instance, thecombined direct and indirect effects of anthropogenic trace gas emissions.Key words. Atmospheric compositionand structure (middle atmosphere – composition and chemistry) – Meteorologyand atmospheric dynamics (general circulation; middle atmosphere dynamics)
机译:介绍了耦合的气候化学模型ECHAM4.L39(DLR)/ CHEM,它可以同时处理气象学和大气化学及其反馈。这是第一个将普通循环模型与化学模型交互结合的模型,它采用了描述平流层和对流层臭氧化学所必需的大多数重要反应和物种,并且计算速度足够快,可以与当前可用的计算机资源进行长期集成。这是可能的,因为用于化学的模型时间步长可以选择为动力学的积分时间步长一样大。在垂直方向上,大气从地面到以10 hPa为中心的顶层离散了39个层,相对较高的垂直分辨率大约为热带对流层顶700 mn。我们提出了代表最近情况的控制模拟结果(1990年),并将其与可用的观测结果进行了比较。重点是研究与描述平流层臭氧层有关的平流层动力学和化学性质。 ECHAM4.L39(DLR)/ CHEM再现了北极涡区平流层动力学的主要特征,包括平流层变暖事件。与早期的模型版本相比,这是一个重大改进。但是,南极环流和温度方面的明显缺陷仍然存在。根据观察结果模拟了臭氧层的季节和年际变化。再现了极地平流层涡旋中氯的活化和失活及其半球间差异。将甲烷氧化视为动态化学反馈的一部分,可以改善平流层水蒸气浓度的空间分布。当前模型是研究例如人为痕量气体排放的直接和间接联合影响的有力工具。 关键词。 大气成分和结构(中间大气–组成和化学)–气象和大气动力学(一般循环;中间大气动力学)

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