激光雷达对气溶胶负荷的观测扩展到整个对流层

A. Deleva, Z. Peshev, T. Dreischuh, D. Stoyanov
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引用次数: 2

摘要

2009年4月至7月,利用Nd: yag激光雷达监测了影响保加利亚索非亚市(42.65 N, 23.38 E)大气的持久气溶胶/粉尘负荷。这些事件几乎贯穿了整个时期。本研究仅关注4月15日和23日获得的实验结果,当时在高度(高达15公里)检测到异常气溶胶层。两天来,巴塞罗那超级计算中心提供的沙尘区域大气模型预测了撒哈拉沙尘对保加利亚的入侵。利用混合单粒子拉格朗日积分轨迹模型计算了激光雷达探测到的气溶胶层的起源。测量结果以大气后向散射系数的时间平均垂直剖面和高时坐标的彩色图表示,这些测量结果说明了所记录的稳定层内气溶胶-质量的空间分布及其时间演变。在两个激光雷达波长(532 nm和1064 nm)检索的剖面被用来计算与后向散射相关的Ǻngström指数的相应剖面,作为观测层中主要气溶胶粒径分数的定性指标。
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Lidar observations of aerosol loadings extended throughout the troposphere
Durable aerosol/dust loadings affecting the atmosphere over the city of Sofia, Bulgaria (42.65 N, 23.38 E) were monitored by a Nd:YAG-laser-based lidar, from April to July 2009. The events lasted almost throughout the entire period. This study is only focused on the experimental results obtained on 15 and 23 April, when extraordinary in altitude (up to 15 km) aerosol layers were detected. For the two days, Dust Regional Atmospheric Model, provided by the Barcelona Super-Computing Center, had forecast Saharan dust incursions over Bulgaria. The origin of the aerosol layers detected by the lidar was identified using the Hybrid Single-Particle Lagrangian Integrated Trajectory model for calculations of the backward air-mass trajectories. The results of measurements are presented in terms of time-averaged vertical profiles of the atmospheric backscatter coefficient and color maps in height-time coordinates, which illustrate the aerosol-mass spatial distribution and its temporal evolution, within the stable layers registered. Retrieved profiles at the two lidar wavelengths (532 nm and 1064 nm) are used to calculate the corresponding profiles of the backscatter-related Ǻngström exponent as a qualitative indicator of the dominant aerosol particle size fractions in the layers observed.
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