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首页> 外文期刊>Atmospheric environment >Nocturnal, seasonal and intra-annual variability of tropospheric aerosols observed using ground-based and space-borne lidars over a tropical location of India
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Nocturnal, seasonal and intra-annual variability of tropospheric aerosols observed using ground-based and space-borne lidars over a tropical location of India

机译:在印度的热带地区使用地面和星载激光雷达观测到的对流层气溶胶的夜间,季节性和年内变化

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摘要

The nocturnal, seasonal and intra-annual variation of vertical distribution of tropospheric aerosols over two nearby stations Gadanki (13.5 degrees N, 79.2 degrees E) and Tirupati (13.6 degrees N, 79.4 degrees E) is investigated using ground-based Micro Pulse Lidar (MPL) and space-borne Lidar (CALIPSO) systems during 2010-2017. The nocturnal variation of aerosol extinction (AE) coefficient reveal high AE below similar to 2 km in midnight hours and aerosols are slowly descending towards the surface during early morning hours. From the seasonal variation, AE values are found to be higher at lower altitudes (<2 km) during winter and post-monsoon seasons, a sharp decrease with increasing altitude is found in tandem with boundary layer and low wind speeds. Interestingly, during monsoon season, significant aerosol loading is found in the altitude range of similar to 2-5.5 km mainly due to the influence of strong Low Level Jet (LLJ). The clean environment observed below similar to 2 km during this season is attributed to the wet scavenging, downward vertical winds and existance of no strong local source. The seasonal mean AE profile derived from CALIPSO matches well with the MPL in all the seasons except in monsoon season where a large bias is noticed below 2 km. The intra-annual variation revealed more than 80% of aerosols existing above (below) the boundary layer during monsoon (winter) months contribute to the total Aerosol Optical Depth (AOD). The depolarization ratio (>0.2) in the month of July shows the dominance of dust particles which includes long-range transport over this locations. Back trajectories reveals that potential sources are changing from season to season at different altitudes and confirms that the aerosols observed at higher altitudes are advected from other land and oceanic regions. Thus, aerosol vertical distribution is mainly controlled by meteorology and dynamics over this region. Further, the reasonably good correlation found between MPL and MODIS AODs suggests that MODIS could provide reliable AOD over land region also.
机译:使用地面微脉冲激光雷达(Gadarki)(北纬13.5度,东经79.2度)和蒂鲁伯蒂(北纬13.6度,东经79.4度)研究了附近两个对流站对流层气溶胶垂直分布的夜间,季节性和年内变化。 MPL)和星载激光雷达(CALIPSO)系统(2010-2017年)。夜间气溶胶消光(AE)系数的变化表明,在午夜时分内,AE值低于2 km,且在清晨时分,气溶胶缓慢地向地面下降。从季节变化来看,冬季和季风后季节的较低海拔(<2 km)的AE值较高,随着边界层和低风速的增加,AE值随海拔的升高而急剧下降。有趣的是,在季风季节,在大约2-5.5 km的高度范围内发现了大量的气溶胶负荷,这主要是由于强大的低空急流(LLJ)的影响。在这个季节,在下面大约2 km处观察到的清洁环境归因于湿扫气,垂直下风和不存在强大的本地源。 CALIPSO得出的季节性平均AE分布在所有季节都与MPL很好地匹配,除了季风季节,在2 km以下发现有较大偏差。年内变化表明,在季风(冬季)月份,边界层以上(以下)存在的气溶胶中,有80%以上是总气溶胶光学深度(AOD)的贡献。 7月的去极化率(> 0.2)显示了尘埃颗粒占主导地位,其中包括该位置的远距离传输。反向轨迹表明,不同海拔高度的潜在气源在每个季节都在变化,并证实在更高海拔高度观测到的气溶胶是从其他陆地和海洋区域移走的。因此,气溶胶垂直分布主要受该地区的气象和动力学控制。此外,在MPL和MODIS AOD之间发现的合理良好的相关性表明,MODIS也可以在陆地区域提供可靠的AOD。

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