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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Springtime transitions of NO2, CO, and O3 over North America: Model evaluation and analysis
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Springtime transitions of NO2, CO, and O3 over North America: Model evaluation and analysis

机译:春天过渡的NO2、CO和O3结束北美:模型评估和分析

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Surface observations from AIRNow and Southeastern Aerosol Research and Characterization Study networks, aircraft observations from the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft program, ozonesondes, and remote sensing measurements from Global Ozone Mapping Experiment, Total Ozone Mapping Spectrometer (TOMS), and Stratospheric Aerosol and Gas Experiment (SAGE) II for February–May 2000 over North America are used to characterize the springtime transitions of O3 and its precursors. These measurements provide a comprehensive data set to evaluate the performance of the 3-D Regional Chemical Transport Model (REAM). The model is then applied to analyze the key factors affecting the springtime transitions of trace gas concentrations and export. The global GEOS-CHEM model is used to provide chemical initial and boundary conditions. Generally, the model results are in good agreement with the observations in the troposphere except for a low bias of upper tropospheric O3; the bias decreases toward the summer and lower latitudes. The rate of observed surface O3 increase in spring is simulated well by REAM. It is overestimated by GEOS-CHEM over the eastern United States. A key factor driving the model difference is daytime mixing depth. A shallow boundary layer in REAM leads to more efficient removal of radicals and hence slower activation of photochemistry in spring, when the primary radical source is relatively small. Comparison of top-down estimates of fossil fuel NOx emissions between REAM and GEOS-CHEM shows model dependence. The associated uncertainty is up to 20% on a monthly basis. Averaging over a season reduces this uncertainty. While tropospheric column NO2 decreases over the continent, it increases over the western North Atlantic due to lightning NOx production. Consequently, the REAM model simulates significant increases of tropospheric O3 over the region as indicated by column data derived from TOMS-SAGE II. Lightning impact is also evident in model-simulated NOx exports.
机译:表面观察AIRNow和东南部气溶胶的研究和表征研究网络,飞机的观察测量臭氧和水蒸气的空客在职飞机项目、臭氧探测仪遥感测量从全球臭氧映射的实验中,臭氧总量的映射光谱仪(汤姆斯)和平流层气溶胶和气体实验(SAGE) 2月中2000年在北美用于描述O3和它的春天过渡体细胞。综合数据集来评估三维区域化学的性能运输模型(令)。分析关键影响因素春天的微量气体的转换浓度和出口。模型是用来提供初始和化学边界条件。是在良好的协议与观察除了低对流层上层的偏见对流层O3;夏天,低纬度地区。表面O3增加弹簧模拟令。美国东部。混合模型的区别是白天的深度。浅边界层令会导致更多有效清除自由基,因此放缓激活的光化学在春天,当主要激进来源相对较小。比较的自上而下的估算的化石燃料令和GEOS-CHEM节目之间的氮氧化物排放模型的依赖。每月20%。赛季减少这种不确定性。对流层列NO2在降低西北大陆,它增加大西洋由于闪电氮氧化物产量。因此,令模型模拟对流层O3的显著增加地区由列数据来源于表示TOMS-SAGE II。模型模拟氮氧化物出口。

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