首页> 外文OA文献 >Ozone et transport dans la haute troposphère tropicale de l’Océan Indien et de l’Asie du Sud : apport des données spatiales (IASI) et de la modélisation
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Ozone et transport dans la haute troposphère tropicale de l’Océan Indien et de l’Asie du Sud : apport des données spatiales (IASI) et de la modélisation

机译:印度洋和南亚热带对流层中的臭氧和运输:空间数据(IASI)和模拟的贡献

摘要

To better understand the processes controling for the distribution of upper tropospheric (UT) ozone (O3) in the tropics, this thesis examines different aspects of pollution transport from sources regions to UT level, through two case studies that take place in the still debated issues.. First study is based on IASI space observations identified an event of transport of UT enriched O3 air masses from Africa to India. During the pre-monsoon season, events of O3 enrichment in UT above the Indian Ocean were essentially attributed to stratospherics intrusions. Simulations have been used to determine its origin, it excludes a stratospheric origin for the event and indicates a probable important contribution by lightning (LiNOx) that occurs over Africa regions. This study could be extended to the whole region and other seasons with a focus on the spring season in order to complete the conclusions obtained during the INDOEX program. The second part focuses on the characterisation of the impact of a deep convective system upon the UTLS composition during the asian summer monsoon. Simulation with a passive tracer highlights the potential of the convective system located over the central Himalaya foothills, to uplift polluted air masses in UTLS to 100 hPa, where the pollutants are rapidly transported by the asian monsoon anticyclone circulation. In agreement with transport pipe towards the UTLS identified by Bergman et al. 2013. However simulation including reactive chemistry show an overestimation by the model of the amount of LiNOx produced, so an adjustment of their parameterization must be made and sensitivity analysis are foreseen to determine precisely O3 production. This study is established in connection with actual major problematic at the center of general debate of the international collaboration. Like ACAM (Atmospheric Composition and the Asian Monsoon) whose targeting the complexe interaction of asian summer monsoon to atmospheric dynamics and chemistry, as well as climate change impact.
机译:为了更好地理解控制热带对流层上空对流层臭氧(O3)分布的控制过程,本论文通过两个仍在争论不休的问题进行的案例研究,考察了从源区到UT水平的污染物输送的不同方面。 ..第一项研究是基于IASI的空间观测结果,确定了富含UT的O3空气团从非洲向印度的运输事件。在季风前季节,印度洋上方UT的O3富集事件主要归因于平流层侵入。模拟已被用来确定其起源,它排除了该事件的平流层起源,并表明了在非洲地区发生的雷电(LiNOx)可能做出的重要贡献。这项研究可以扩展到整个地区和其他季节,重点放在春季,以完成在INDOEX计划中获得的结论。第二部分重点介绍了亚洲夏季风期间深对流系统对UTLS组成的影响的特征。用被动示踪剂进行的模拟突出显示了位于喜马拉雅山中部丘陵上空的对流系统的潜力,可以将UTLS中的污染气团提升至100 hPa,亚洲季风反气旋环流将污染物迅速转移。在与通往Bergman等人确定的UTLS的运输管道达成协议后, 2013年。然而,包括反应化学在内的模拟结果表明,该模型高估了LiNOx的产生量,因此必须对其参数进行调整,并进行灵敏度分析以准确确定O3的产生。这项研究是在国际合作一般辩论的中心针对实际的重大问题而建立的。就像ACAM(大气成分和亚洲季风)一样,其目标是亚洲夏季风与大气动力学和化学作用以及气候变化影响之间的复杂相互作用。

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    Tocquer Flore;

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  • 年度 2015
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