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Off-line algorithm for calculation of vertical tracer transport in the troposphere due to deep convection

机译:深度对流引起的对流层垂直示踪剂传输的离线算法

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摘要

A modified cumulus convection parametrisation scheme is presented.This scheme computes the mass of air transported upward in a cumulus cellusing conservation of moisture and a detailed distribution of convectiveprecipitation provided by a reanalysis dataset. The representation ofvertical transport within the scheme includes entrainment and detrainmentprocesses in convective updrafts and downdrafts. Output from the proposedparametrisation scheme is employed in the National Institute forEnvironmental Studies (NIES) global chemical transport model driven byJRA-25/JCDAS reanalysis. The simulated convective precipitation rate andmass fluxes are compared with observations and reanalysis data. A simulationof the short-lived tracer Rn is used to further evaluate theperformance of the cumulus convection scheme. Simulated distributions ofRn are evaluated against observations at the surface and in the freetroposphere, and compared with output from models that participatedin the TransCom-CH Transport Model Intercomparison. From thiscomparison, we demonstrate that the proposed convective scheme in general isconsistent with observed and modeled results.
机译:提出了一种改进的积云对流参数化方案,该方案利用水分守恒和重新分析数据集提供的详细对流降水来计算积云细胞中向上输送的空气质量。该方案中垂直运输的表示包括对流上升气流和下降气流中的夹带和减气过程。拟议的参数化方案的输出用于由JRA-25 / JCDAS重新分析驱动的美国国家环境研究所(NIES)全球化学迁移模型。将模拟的对流降水率和质量通量与观测值和再分析数据进行比较。短期示踪剂Rn的模拟用于进一步评估积云对流方案的性能。对照表面和自由对流层的观测值评估Rn的模拟分布,并将其与参与TransCom-CH传输模型比较的模型的输出进行比较。通过这种比较,我们证明了所提出的对流方案总体上与观测和模拟结果一致。

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