喜马拉雅气溶胶工厂的影响:喜马拉雅山谷上纯生物成核的高分辨率数值模拟结果。

IF 3.3 3区 化学 Q2 CHEMISTRY, PHYSICAL
Giancarlo Ciarelli, Arineh Cholakian, Manuel Bettineschi, Bruno Vitali, Bertrand Bessagnet, Victoria A Sinclair, Johannes Mikkola, Imad El Haddad, Dino Zardi, Angela Marinoni, Alessandro Bigi, Paolo Tuccella, Jaana Bäck, Hamish Gordon, Tuomo Nieminen, Markku Kulmala, Douglas Worsnop, Federico Bianchi
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引用次数: 0

摘要

2014年12月在尼泊尔珠峰大本营收集的观测数据表明,纯生物成因的新粒子形成事件频繁发生。据推测,这些事件是由连接印度恒河平原和观测地点尼泊尔气候观测站金字塔的山谷中形成的沿山谷风控制的。山谷风将生物成因的高氧有机分子输送到海拔较高的地方,在那里它们形成核。该机制被称为“喜马拉雅气溶胶工厂”。其地理范围和气候影响目前尚不清楚。鉴于此,我们进行了数值化学模型模拟,以证实该机制的存在,并量化其地理范围。我们的数值模拟证实,位于山谷中的生物源排放物可以转化为超低挥发性有机化合物,通过沿山谷的风输送到观测地点,并在那里成核。从生物源排放物释放到转化为超低挥发性有机化合物,再到到达观测地点的总体时间尺度约为4小时,与预测的沿谷风强度和生物源排放物的地理分布一致。对生物成因粒子和高氧有机分子的最大注入高度的初步估计表明,在海拔高达5000-6000 m a.s.l的地方存在有效成核气体和生物成因粒子。这些结果表明,在特定的天气条件下,喜马拉雅链是自由对流层生物成因气溶胶负荷的主要贡献者。考虑到这些发现,我们强烈鼓励实地考察活动,特别是在山谷底部的入口,以及支持亚洲山区大气研究的研究联盟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The impact of the Himalayan aerosol factory: results from high resolution numerical modelling of pure biogenic nucleation over the Himalayan valleys.

Observational data collected in December 2014 at the base camp of Mount Everest, Nepal, indicated frequent new particle formation events of pure biogenic origin. Those events were speculated to be controlled by the along-valley winds forming in the valley connecting the Indo-Gangetic plain to the observational site, the Nepal Climate Observatory-Pyramid. The valley winds funnel highly oxygenated organic molecules of biogenic origin to higher elevations where they nucleate. The mechanism was referred to as "The Himalayan aerosol factory". Its geographical extent and climate implications are currently unknown. In view of this, we conducted numerical chemical model simulations to corroborate the presence of the mechanism, and to quantify its geographical extent. Our numerical simulations confirmed that biogenic emissions located in the valleys can be converted into ultra-low volatility organic compounds, transported to the observational site by the along-valley winds, and therein nucleate. The overall time scale of the process, from the release of biogenic emissions to the conversion to ultra-low volatile organic compounds to the arrival time at the observational site, was found to be around 4 hours, consistent with the predicted along-valley winds intensity and the geographical distribution of biogenic emissions. A first estimation of the maximum injection height of biogenic particles, and highly oxygenated organic molecules, indicated the presence of efficient nucleating gases and biogenic particles at an elevation as high as 5000-6000 m a.s.l. These results suggest that the Himalayan chain, under specific weather conditions, is a main contributor to the biogenic aerosol loads in the free troposphere. Considering these findings, field campaigns, especially at the entrance of the valley's floors, and research consortia supporting atmospheric research in Asian mountain regions, are highly encouraged.

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来源期刊
Faraday Discussions
Faraday Discussions 化学-物理化学
自引率
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259
期刊介绍: Discussion summary and research papers from discussion meetings that focus on rapidly developing areas of physical chemistry and its interfaces
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