The relationship between cloud condensation nuclei (CCN) concentration and light extinction of dried particles: indications of underlying aerosol processes and implications for satellite-based CCN estimates
The relationship between cloud condensation nuclei (CCN) concentration and light extinction of dried particles: indications of underlying aerosol processes and implications for satellite-based CCN estimates
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DOI:
10.5194/acp-15-7585-2015
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发表时间:
2015-07
影响因子:
6.3
通讯作者:
Y. Shinozuka;A. Clarke;A. Nenes;A. Jefferson;R. Wood;C. McNaughton;J. Ström;P. Tunved;J. Redemann;K. Thornhill;R. Moore;T. Lathem;Jack J. Lin;Y. Yoon
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文献类型:
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作者:
Y. Shinozuka;A. Clarke;A. Nenes;A. Jefferson;R. Wood;C. McNaughton;J. Ström;P. Tunved;J. Redemann;K. Thornhill;R. Moore;T. Lathem;Jack J. Lin;Y. Yoon
Abstract. We examine the relationship between the number concentration of boundary-layer cloud condensation nuclei (CCN) and light extinction to investigate underlying aerosol processes and satellite-based CCN estimates. For a variety of airborne and ground-based observations not dominated by dust, regression identifies the CCN (cm−3) at 0.4 ± 0.1% supersaturation with 100.3α +1.3σ0.75 where σ (Mm−1) is the 500 nm extinction coefficient by dried particles and α is the Angstrom exponent. The deviation of 1 km horizontal average data from this approximation is typically within a factor of 2.0. ∂logCCN / ∂logσ is less than unity because, among other explanations, growth processes generally make aerosols scatter more light without increasing their number. This, barring special meteorology–aerosol connections, associates a doubling of aerosol optical depth with less than a doubling of CCN, contrary to previous studies based on heavily averaged measurements or a satellite algorithm.