气溶胶
环境科学
云计算
云凝聚核
卫星
液态水通道
海盐气溶胶
液态水含量
大气科学
气象学
遥感
冷凝
遮罩(插图)
地质学
地理
物理
计算机科学
视觉艺术
艺术
操作系统
海盐
天文
作者
Peter Manshausen,Duncan Watson‐Parris,Matthew W. Christensen,Jukka-Pekka Jalkanen,Philip Stier
出处
期刊:Nature
[Springer Nature]
日期:2022-10-05
卷期号:610 (7930): 101-106
被引量:59
标识
DOI:10.1038/s41586-022-05122-0
摘要
Abstract Cloud reflectivity is sensitive to atmospheric aerosol concentrations because aerosols provide the condensation nuclei on which water condenses 1 . Increased aerosol concentrations due to human activity affect droplet number concentration, liquid water and cloud fraction 2 , but these changes are subject to large uncertainties 3 . Ship tracks, long lines of polluted clouds that are visible in satellite images, are one of the main tools for quantifying aerosol–cloud interactions 4 . However, only a small fraction of the clouds polluted by shipping show ship tracks 5,6 . Here we show that even when no ship tracks are visible in satellite images, aerosol emissions change cloud properties substantially. We develop a new method to quantify the effect of shipping on all clouds, showing a cloud droplet number increase and a more positive liquid water response when there are no visible tracks. We directly detect shipping-induced cloud property changes in the trade cumulus regions of the Atlantic, which are known to display almost no visible tracks. Our results indicate that previous studies of ship tracks were suffering from selection biases by focusing only on visible tracks from satellite imagery. The strong liquid water path response we find translates to a larger aerosol cooling effect on the climate, potentially masking a higher climate sensitivity than observed temperature trends would otherwise suggest.
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