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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >An idealized stratospheric model useful for understanding differences between long-lived trace gas measurements and global chemistry-climate model output
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An idealized stratospheric model useful for understanding differences between long-lived trace gas measurements and global chemistry-climate model output

机译:理想的平流层模型,可用于了解长期痕量气体测量值与全球化学气候模型输出之间的差异

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摘要

We use a modified version of the tropical leaky pipe (TLP) model of the stratosphere to explore how well an idealized model can (1) reproduce global chemistry-climate model (CCM) output and (2) constrain transport characteristics necessary to replicate measurements of long-lived trace gases. The version of the TLP model we use includes the simulation of long-lived trace gases, such as SF6 and CO_2, as well as photochemically active trace gases such as CFC-11, CFC-12, and N_2O. The TLP model was found to accurately replicate trace gas output from the Canadian Middle Atmosphere Model (CMAM) for time-averaged profiles in the tropics and each extratropical region. Given confidence that the TLP model represents the basic transport features in CMAM we then used the TLP model to interpret differences between CMAM output and measurements from the Atmospheric Chemistry Experiment and balloons. The TLP model is shown to uniquely determine residual mean circulation and recirculation (mixing between the extratropics and tropics) changes necessary for CMAM to more accurately simulate the measurements. Such guidance on these transport parameters is novel due to the relatively high precision and the simultaneous derivation of important parameters, as compared to previous studies. The TLP model can ideally be used as a bridge between measurements and CCMs to potentially allow more targeted modification of the CCMs than would otherwise be possible.
机译:我们使用平流层热带漏水管(TLP)模型的修改版来探索理想化模型能够(1)再现全球化学-气候模型(CCM)输出的良好程度,以及(2)约束重复测量的必要运输特征。长寿命的微量气体。我们使用的TLP模型版本包括长寿命痕量气体(例如SF6和CO_2)以及光化学活性痕量气体(例如CFC-11,CFC-12和N_2O)的模拟。人们发现,TLP模型可以准确地复制加拿大中层大气模型(CMAM)的痕量气体输出,以用于热带地区和每个热带地区的时间平均剖面。确信TLP模型代表了CMAM中的基本运输特征,然后我们使用TLP模型来解释CMAM输出与大气化学实验和气球测量值之间的差异。 TLP模型显示出可以唯一确定CMAM能够更准确地模拟测量结果所需的平均剩余循环和再循环(温带和热带之间的混合)变化。与以前的研究相比,由于相对较高的精度和同时推导重要参数,因此对这些传输参数的指导是新颖的。理想地,TLP模型可以用作测量和CCM之间的桥梁,以潜在地允许比其他方式更有针对性地修改CCM。

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