首页> 外文期刊>Bulletin of the American Meteorological Society >Overview of the CPOC Pilot Study at Whiteface Mountain, NY Cloud Processing of Organics within Clouds (CPOC)
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Overview of the CPOC Pilot Study at Whiteface Mountain, NY Cloud Processing of Organics within Clouds (CPOC)

机译:白面山区的CPOC试点研究概述,云云(CPOC)有机体云加工

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Aqueous chemical processing within cloud and fog water is thought to be a key process in the production and transformation of secondary organic aerosol mass, found abundantly and ubiquitously throughout the troposphere. Yet, significant uncertainty remains regarding the organic chemical reactions taking place within clouds and the conditions under which those reactions occur, owing to the wide variety of organic compounds and their evolution under highly variable conditions when cycled through clouds. Continuous observations from a fixed remote site like Whiteface Mountain (WFM) in New York State and other mountaintop sites have been used to unravel complex multiphase interactions in the past, particularly the conversion of gas-phase emissions of SO2 to sulfuric acid within cloud droplets in the presence of sunlight. These scientific insights led to successful control strategies that reduced aerosol sulfate and cloud water acidity substantially over the following decades. This paper provides an overview of observations obtained during a pilot study that took place at WFM in August 2017 aimed at obtaining a better understanding of Chemical Processing of Organic Compounds within Clouds (CPOC). During the CPOC pilot study, aerosol cloud activation efficiency, particle size distribution, and chemical composition measurements were obtained below-cloud for comparison to routine observations at WFM, including cloud water composition and reactive trace gases. Additional instruments deployed for the CPOC pilot study included a Doppler lidar, sun photometer, and radiosondes to assist in evaluating the meteorological context for the below-cloud and summit observations.
机译:云和雾水中的水化学过程被认为是二次有机气溶胶质量产生和转化的关键过程,二次有机气溶胶在对流层中广泛存在。然而,由于有机化合物种类繁多,以及它们在云层中循环时在高度可变的条件下的演化,云层中发生的有机化学反应以及这些反应发生的条件仍然存在很大的不确定性。过去,在纽约州的怀特法斯山(Whiteface Mountain,WFM)等固定偏远地点和其他山顶地点进行的连续观测被用来揭示复杂的多相相互作用,特别是在阳光照射下,云滴内SO2气相排放转化为硫酸的过程。这些科学见解导致了成功的控制策略,在接下来的几十年里大幅降低了气溶胶硫酸盐和云水酸度。本文概述了2017年8月在WFM进行的一项试点研究期间获得的观测结果,该研究旨在更好地了解云中有机化合物的化学过程(CPOC)。在CPOC试点研究期间,在云层下方获得了气溶胶云激活效率、粒度分布和化学成分测量值,以与WFM的常规观测结果进行比较,包括云水成分和反应性痕量气体。CPOC试点研究部署的其他仪器包括多普勒激光雷达、太阳光度计和无线电探空仪,以帮助评估云层下和山顶观测的气象背景。

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