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Seasonal variation of near surface black carbon and satellite derived vertical distribution of aerosols over a semi-arid station in India

机译:印度半干旱地区近地表黑碳的季节性变化和卫星衍生的气溶胶垂直分布

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Extensive measurements of aerosol black carbon mass concentration (BC) and vertical profiles of atmospheric aerosols have been carried out using Aethalometer and CALIPSO level - 2 satellite data from December 2012 to November 2014 over a semi-arid station, Anantapur. We found a bimodal distribution in the mass concentrations of BC aerosols on a diurnal scale. A sharp peak was observed during morning rush hours (7:00 to 8:00 LT) almost an hour after the local sunrise. After which, a broad nocturnal peak was found during similar to 21:00 to 22:00 LT. The seasonal mean BC concentrations (Mixed layer height (M-L)) were found to be 3.45 +/- 1.44 mu g/m(3) (676 +/- 117 m), 2.55 +/- 0.85 mu g/m(3) (1215 +/- 190 m), 1.22 +/- 0.31 mu g/m(3) (1134 +/- 194 m) and 1.75 +/- 0.70 mu g/m(3) (612 +/- 135 m), during the winter, summer, monsoon and post-monsoon respectively. The vertical profiles of aerosol extinction coefficient and back scattering ratio profiles were derived from Cloud Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) showed a strong seasonal variation with aerosols mostly confined below 2 km during the post-monsoon and winter seasons whereas in the other two seasons, the aerosol layer expands beyond 6 km. Depolarization ratios (>0.2) are higher during summer and monsoon at higher altitude regions demonstrate the presence of dust particles, which contribute to the large aerosol extinction at higher levels. These results are further supported by the backward trajectory cluster analysis. (C) 2016 Elsevier B.V. All rights reserved.
机译:2012年12月至2014年11月,使用半干旱站Anantapur使用Aethalometer和CALIPSO 2级卫星数据对气溶胶黑碳质量浓度(BC)和大气气溶胶的垂直剖面进行了广泛的测量。我们发现昼夜尺度上BC气溶胶的质量浓度呈双峰分布。当地日出后近一个小时,在高峰时段(美国中部时间7:00至8:00)观察到一个尖峰。此后,在大约21:00至22:00 LT期间发现了一个宽的夜间活动高峰。发现季节性平均BC浓度(混合层高度(ML))为3.45 +/- 1.44μg / m(3)(676 +/- 117 m),2.55 +/- 0.85μg / m(3) (1215 +/- 190 m),1.22 +/- 0.31μg / m(3)(1134 +/- 194 m)和1.75 +/- 0.70μg / m(3)(612 +/- 135 m) ,分别在冬季,夏季,季风和季风后。气溶胶消光系数和反向散射比的垂直剖面图来自云气溶胶激光雷达和红外探路者卫星观测(CALIPSO),显示出强烈的季节性变化,在季风后和冬季,气溶胶大多被限制在2 km以下,而在其他季节两个季节,气溶胶层扩展超过6公里。在夏季和高海拔地区的季风期间,去极化率较高(> 0.2),这表明存在粉尘颗粒,这些粉尘颗粒在较高浓度下导致大量的气溶胶消光。这些结果得到反向轨迹聚类分析的进一步支持。 (C)2016 Elsevier B.V.保留所有权利。

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