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Aerosol impacts on warm-cloud microphysics and drizzle in a moderately polluted environment

机译:气溶胶对暖云微妙和毛毛雨的影响,在适度污染的环境中

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摘要

Climate is critically affected by aerosols, which alter cloud lifecycles and precipitation distribution through radiative and microphysical effects. In this study, aerosol and cloud property datasets from MODIS (Moderate Resolution Imaging Spectroradiometer), onboard the Aqua satellite, and surface observations, including aerosol concentrations, raindrop size distribution, and meteorological parameters, were used to statistically quantify the effects of aerosols on low-level warm-cloud microphysics and drizzle over northern Taiwan during multiple fall seasons (from 15?October to 30?November of 2005–2017). Our results indicated that northwestern Taiwan, which has several densely populated cities, is dominated by low-level clouds (e.g., warm, thin, and broken clouds) during the fall season. The observed effects of aerosols on warm clouds indicated aerosol indirect effects (i.e., increased aerosol loading caused a decrease in cloud effective radius (CER)), an increase in cloud optical thickness, an increase in cloud fraction, and a decrease in cloud-top temperature under a fixed cloud water path. Quantitatively, aerosol–cloud interactions ( ACI = - ? ln CER ? ln α | CWP , changes in CER relative to changes in aerosol amounts) were 0.07 for our research domain and varied between 0.09 and 0.06 in the surrounding remote (i.e., ocean) and polluted (i.e., land) areas, respectively, indicating aerosol indirect effects were stronger in the remote area. From the raindrop size distribution analysis, high aerosol loading resulted in a decreased frequency of drizzle events, redistribution of cloud water to more numerous and smaller droplets, and reduced collision–coalescence rates. However, during light rain ( ≤1 ?mm?h ?1 ), high aerosol concentrations drove raindrops towards smaller droplet sizes and increased the appearance of drizzle drops. This study used long-term surface and satellite data to determine aerosol variations in northern Taiwan, effects on clouds and precipitation, and observational strategies for future research on aerosol–cloud–precipitation interactions.
机译:气候受气溶胶受气溶胶的影响,通过辐射和微手术作用改变云生命周期和降水分布。在本研究中,来自MODIS的气溶胶和云属性数据集(中等分辨率成像光谱仪),船上卫星和表面观察,包括气溶胶浓度,雨水尺寸分布和气象参数,用于统计量化气溶胶对低温的影响 - 在多个秋季季节(从15岁到30月30日到30月30日),暖云微软和台湾北部的毛毛雨,毛毛雨我们的结果表明,台湾拥有若干密集的城市的西北部,在秋季期间由低级云(例如,温暖,薄,破碎的云)主导。观察到气溶胶对暖云的影响表明气溶胶间接效应(即,增加的气溶胶载量导致云有效半径(CER)的降低,云光学厚度的增加,云分数的增加,以及云层的减少固定云水道下的温度。定量地,天空云相互作用(ACI = - α1NCER?LNα1| CWP相对于气溶胶量的变化,CER的变化)为我们的研究结构域为0.07,而周围偏远的周围(即海洋)在0.09和0.06之间变化分别污染(即土地)区域,表明偏远地区的气溶胶间接影响更强。从雨滴尺寸分布分析中,高气溶胶载量导致毛毛雨事件的频率下降,云水再分布到更多且较小的液滴,降低碰撞聚结率。然而,在小雨期间(≤1≤1ΩΩh?1),高气溶胶浓度使雨滴朝向更小的液滴尺寸并增加了淋雨的外观。本研究使用了长期表面和卫星数据来确定台湾北部的气溶胶变化,对云层和降水的影响,以及未来气溶胶云降水相互作用的研究的观测策略。

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