Retrievals of dust-related particle mass and ice-nucleating particle concentration profiles with ground-based polarization lidar and sun photometer over a central China megacity

Yun He, Yunfei Zhang, Fuchao Liu, Zhenping Yin, Yang Yi, Yifan Zhan, F. Yi
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Abstract

Abstract. The POLIPHON (Polarization Lidar Photometer Networking) method is a powerful pathway to retrieve the height profiles of dust-related particle mass and ice-nucleating particles (INP) concentrations. The conversion factors fitted from the sun photometer observation data are the major part of the POLIPHON computations, which can convert the polarization-lidar-derived dust extinction coefficients into the dust-related particle mass and INP concentrations. For a central China megacity Wuhan (30.5° N, 114.4° E), located at the downstream area several thousands of kilometers far away from the source regions of Asian dust, dust particles always mix with other aerosols from local emission. Therefore, very few dust case data sets can be available when using the column-integrated Angstrom exponent (for 440–870 nm)  0.1 recorded by sun photometer as the filtering criteria. Instead, we present another dust-case data-set screening scheme that applies the simultaneous polarization lidar observation to verify the occurrence of dust. Based on the 33 dust-intrusion days identified during 2011–2013, the extinction-to-volume (cv,d) and extinction-to-large particle (with radius > 250 nm) number concentration (c250,d) conversion factors are determined to be 0.52 × 10−12 Mm m3 m−3 and 0.11 Mm cm−3, respectively. They are both smaller than those observed at Lanzhou SACOL (36.0° N, 104.1° E), a site closer to the Gobi Desert, due to the partial dust sedimentation during transport. The conversion factors are applied in a dust event in Wuhan to reveal the typical dust-related INP concentration over East Asia city. The proposed dust-case data-set screening scheme may potentially be extended to the other polluted city sites more influenced by mixed dust.
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基于地基偏振激光雷达和太阳光度计的中国中部特大城市尘埃相关粒子质量和冰核粒子浓度剖面反演
摘要偏振激光雷达光度计网络(POLIPHON)方法是获取尘埃相关粒子质量和冰核粒子(INP)浓度高度分布的有力途径。由太阳光度计观测数据拟合的转换因子是POLIPHON计算的主要部分,它可以将偏振激光雷达导出的尘埃消光系数转换为与尘埃有关的粒子质量和INP浓度。中国中部特大城市武汉(30.5°N, 114.4°E)位于距离亚洲沙尘源区数千公里的下游地区,沙尘颗粒经常与当地排放的其他气溶胶混合。因此,当使用太阳光度计记录的柱积分埃氏指数(440-870 nm) 0.1作为过滤标准时,可获得的沙尘数据集很少。相反,我们提出了另一种沙尘数据集筛选方案,该方案应用同步偏振激光雷达观测来验证沙尘的发生。基于2011-2013年的33个沙尘侵入日,确定了灭绝-体积(cv,d)和灭绝-大颗粒(半径> 250 nm)数浓度(c250,d)的转换因子分别为0.52 × 10−12 Mm m3 m−3和0.11 Mm cm−3。在靠近戈壁沙漠的兰州SACOL(36.0°N, 104.1°E),由于运输过程中的部分沙尘沉降,两者都小于观测值。将转换因子应用于武汉的一次沙尘事件,揭示了东亚城市典型的沙尘相关INP浓度。建议的粉尘数据集筛选方案可能会推广到其他受混合粉尘影响较大的污染城市场地。
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