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首页> 外文期刊>Geoscientific Model Development >The application of the Modified Band Approach for the calculation of on-line photodissociation rate constants in TM5: implications for oxidative capacity
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The application of the Modified Band Approach for the calculation of on-line photodissociation rate constants in TM5: implications for oxidative capacity

机译:修正谱带方法在TM5在线光解离速率常数计算中的应用:对氧化能力的影响

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A flexible and explicit on-line parameterization for the calculation oftropospheric photodissociation rate constants (J-values) has been integratedinto the global Chemistry Transport Model TM5. Here we provide acomprehensive description of this Modified Band Approach (MBA) includingdetails of the optimization procedure employed, the methodology applied forcalculating actinic fluxes, the photochemical reaction data used for eachchemical species, the aerosol climatology which is adopted and theparameterizations adopted for improving the description of scattering andabsorption by clouds. The resulting J-values change markedly throughout thetroposphere when compared to the offline approach used to date, withsignificant increases in the boundary layer and upper troposphere.Conversely, for the middle troposphere a reduction in the actinic fluxresults in a decrease in J-values. Integrating effects shows that applicationof the MBA introduces seasonal dependent differences in important trace gasoxidants. Tropospheric ozone (O3) changes by ±10% in theseasonal mean mixing ratios throughout the troposphere, especially overland. These changes and the perturbations in the photolysis rate of O3induce changes of ±15% in tropospheric OH. In part this is due to anincrease in the re-cycling efficiency of nitrogen oxides. The overallincrease in northern hemispheric tropospheric ozone strengthens theoxidizing capacity of the troposphere significantly and reduces the lifetimeof CO and CH4 by ~5 % and ~4%, respectively. Changesin the tropospheric CO burden, however, are limited to a few percent due tocompeting effects. Comparing the distribution of tropospheric ozone in theboundary layer and middle troposphere against observations in Europe showsthere are improvements in the model performance during boreal winter in theNorthern Hemisphere near regions affected by high nitrogen oxide emissions.Monthly mean total columns of nitrogen dioxide and formaldehyde also comparemore favorably against OMI and SCIAMACHY total column observations.
机译:用于计算对流层光解离速率常数( J 值)的灵活,明确的在线参数化已集成到全球化学运输模型TM5中。在这里,我们对这种改进的谱带方法(MBA)进行了全面的描述,包括所用优化程序的详细信息,用于计算光化通量的方法,用于每种化学物质的光化学反应数据,采用的气溶胶气候学以及为改进描述​​而采用的参数化。云的散射和吸收。与迄今使用的离线方法相比,在整个对流层中生成的 J 值发生显着变化,边界层和对流层上层的显着增加。相反,对流层中层的光化通量减少导致 J 值减小。综合效果表明,MBA的应用在重要的痕量气体氧化剂中引入了季节依赖性。对流层臭氧(O 3 )在整个对流层(尤其是陆上)的季节平均混合比变化±10%。这些变化和O 3 光解速率的扰动导致对流层OH的变化为±15%。部分原因是由于氮氧化物的再循环效率提高。北半球对流层臭氧的整体增加显着增强了对流层的氧化能力,并使CO和CH 4 的寿命分别降低了5%和〜4%。然而,由于竞争效应,对流层一氧化碳负荷的变化被限制在百分之几之内。比较欧洲对流层边界和对流层中对流层臭氧的分布与欧洲的观察结果表明,在北半球受高氮氧化物排放影响的地区的寒冬期间,模型的性能有所改善。月平均二氧化氮和甲醛的总柱数也比较有利针对OMI和SCIAMACHY的总色谱柱观测值。

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