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    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/100766


    Title: What causes observed fog trends: Air quality or climate change?
    Authors: 林能暉;Klemm, Otto;Lin, Neng-Huei
    Contributors: 地球科學學院大氣科學學系
    Date: 2016-05-01
    Issue Date: 2026-04-21 14:13:25 (UTC+8)
    Publisher: AAGR Aerosol and Air Quality Research;Cham: Springer International Publishing
    Abstract: 摘要: Fog is a situation when the visual range, which is the horizontal visibility, is reduced to less than 1000 m near the Earth’s surface by the presence of cloud droplets. Fog trend analyses are reported in the literature for hundreds of stations worldwide, the majority of which showing a considerable reduction of fog. Although fog is often associated with conditions at which cloud condensation nuclei had been activated at rH (relative humidity) > 100% and rapid growth had lead to the formation of fog droplets, this study focusses on urban air masses and conditions when rH is just below 100%. Mie scattering analysis shows that fog can form under such conditions and the reduction of the visual range is mainly caused by submicron aerosol particles which grow to diameters around 1 µm through deliquescence. The liquid water content itself is poorly correlated with the visual range. Assuming equilibrium conditions, both an increase of the air temperature and a reduction of the aerosol particle concentration lead to reductions of fog. In our example case, the increment for a temperature increase by 0.1°C had about the same effect as the reduction of aerosol concentrations by 10%. Care must be taken in projecting this result to actual conditions because the system is non-linear. However, physical evidence is presented which confirms that both climate change and an improvement of air quality are mechanisms that can contribute to the reduction of fog.
    其他題名: Aerosol Air Qual. Res
    出版者: Cham: Springer International Publishing
    出版日期: 2016-05-01
    出處: Aerosol and air quality research, 2016-05, Vol.16 (5), p.1131-1142
    版權: Taiwan Association for Aerosol Research 2016
    識別號: ISSN: 1680-8584
    識別號: ISSN: 2071-1409
    識別號: EISSN: 2071-1409
    識別號: DOI: 10.4209/aaqr.2015.05.0353
    Appears in Collections:[Department of Atmospheric Sciences] journal & Dissertation

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