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Simulation of Tropospheric Ozone with MOZART-2:An Evaluation Study over East Asia

机译:MOZART-2模拟对流层臭氧的东亚评价研究

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摘要

Climate changes induced by human activities have attracted a great amount of attention. With this,a coupling system of an atmospheric chemistry model and a climate model is greatly needed in China for better understanding the interaction between atmospheric chemical components and the climate. As the first step to realize this coupling goal, the three-dimensional global atmospheric chemistry transport model MOZART-2 (the global Model of Ozone and Related Chemical Tracers, version 2) coupled with CAM2 (the Community Atmosphere Model, version 2) is set up and the model results are compared against observations obtained in East Asia in order to evaluate the model performance. Comparison of simulated ozone mixing ratios with ground level observations at Minamitorishima and Ryori and with ozonesonde data at Naha and Tateno in Japan shows that the observed ozone concentrations can be reproduced reasonably well at Minamitorishima but they tend to be slightly overestimated in winter and autumn while underestimated a little in summer at Ryori. The model also captures the general features of surface CO seasonal variations quite well, while it underestimates CO levels at both Minamitorishima and Ryori.The underestimation is primarily associated with the emission inventory adopted in this study. Compared with the ozonesonde data, the simulated vertical gradient and magnitude of ozone can be reasonably well simulated with a little overestimation in winter, especially in the upper troposphere. The model also generally captures the seasonal, latitudinal and altitudinal variations in ozone concentration. Analysis indicates that the underestimation of tropopause height in February contributes to the overestimation of winter ozone in the upper and middle troposphere at Tateno.
机译:人类活动引起的气候变化已引起广泛关注。因此,在中国急需一种大气化学模型与气候模型的耦合系统,以更好地理解大气化学成分与气候之间的相互作用。作为实现这一耦合目标的第一步,设置了三维全球大气化学迁移模型MOZART-2(全球臭氧和相关化学示踪剂模型,版本2)和CAM2(社区大气模型,版本2)。然后将模型结果与在东亚获得的观测结果进行比较,以评估模型性能。模拟的臭氧混合比与在Minamitorishima和Ryori的地面观测值以及在日本Naha和Tateno的臭氧探空仪数据比较表明,在Minamitorishima可以很好地再现观测到的臭氧浓度,但是在冬季和秋季它们会被稍微高估,而被低估夏天在Ryori待会儿。该模型还很好地捕捉了地表CO季节变化的一般特征,同时低估了Minmitorishima和Ryori的CO水平。低估主要与本研究中采用的排放清单有关。与臭氧探空仪的数据相比,在冬季,特别是在对流层上方,模拟的垂直梯度和臭氧强度可以得到很好的模拟,而对冬季的估计则略高。该模型还通常捕获臭氧浓度的季节性,纬度和高度变化。分析表明,2月对流层顶高度的低估造成了Tateno对流层中上层冬季臭氧的高估。

著录项

  • 来源
    《大气科学进展(英文版)》 |2005年第4期|585-594|共10页
  • 作者单位

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;

    Graduate School of the Chinese Academy of Sciences, Beijing 100049;

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;

    State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 大气科学(气象学);
  • 关键词

    tropospheric ozone, global chemical transport model, MOZART-2, tropopause, East Asia;

    机译:对流层臭氧;全球化学迁移模型;MOZART-2;对流层顶;东亚;
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