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热带边界层中的粒子成核及其与海洋硫源的耦合。

Particle nucleation in the tropical boundary layer and its coupling to marine sulfur sources.

作者信息

Clarke AD, Davis D, Kapustin VN, Eisele F, Chen G, Paluch I, Lenschow D, Bandy AR, Thornton D, Moore K, Mauldin L, Tanner D, Litchy M, Carroll MA, Collins J, Albercook G

机构信息

A. D. Clarke, V. N. Kapustin, K. Moore, M. Litchy, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI, USA. D. Davis, F. Eisele, G. Chen, School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atl.

出版信息

Science. 1998 Oct 2;282(5386):89-92. doi: 10.1126/science.282.5386.89.

Abstract

New particle formation in a tropical marine boundary layer setting was characterized during NASA's Pacific Exploratory Mission-Tropics A program. It represents the clearest demonstration to date of aerosol nucleation and growth being linked to the natural marine sulfur cycle. This conclusion was based on real-time observations of dimethylsulfide, sulfur dioxide, sulfuric acid (gas), hydroxide, ozone, temperature, relative humidity, aerosol size and number distribution, and total aerosol surface area. Classic binary nucleation theory predicts no nucleation under the observed marine boundary layer conditions.

摘要

在美国国家航空航天局的太平洋热带探索使命A计划期间,对热带海洋边界层环境中的新粒子形成进行了特征描述。这是迄今为止气溶胶成核和生长与天然海洋硫循环相关的最清晰证明。这一结论基于对二甲基硫、二氧化硫、硫酸(气体)、氢氧根、臭氧、温度、相对湿度、气溶胶粒径和数量分布以及总气溶胶表面积的实时观测。经典二元成核理论预测在观测到的海洋边界层条件下不会发生成核。

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