Nocturnal, seasonal and intra-annual variability of tropospheric aerosols observed using ground-based and space-borne lidars over a tropical location of India. (15th September 2019)

• Record Type: Journal Article
• Authors: Prasad, P.; Raman, M.Roja; Ratnam, M.Venkat; Ravikiran, V.; Madhavan, B.L.; Bhaskara Rao, S. Vijaya
• Is Part Of: Atmospheric environment. Volume 213(2019)
• Page Start: 185
• Page End: 198
• Publication Date: 2019-09-15
• Subjects: Aerosol -- Vertical distribution -- Lidar -- Extinction coefficient -- CALIPSO; Air -- Pollution -- Periodicals; Air -- Pollution -- Meteorological aspects -- Periodicals; 551.51
• DOI: 10.1016/j.atmosenv.2019.06.008
• Languages: English
• ISSNs: 1352-2310

Abstract

Abstract: The nocturnal, seasonal and intra-annual variation of vertical distribution of tropospheric aerosols over two nearby stations Gadanki (13.5 o N, 79.2 o E) and Tirupati (13.6 o N, 79.4 o 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 ∼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 ∼2–5.5 km mainly due to the influence of strong Low Level Jet (LLJ). The clean environment observed below ∼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. Highlights: Lidar observed aerosol vertical distribution over Indian tropical stations show strong nocturnal and seasonal variation. Aerosol extinction over Gadanki/Tirupati region is higher at altitudes <2 km during winter and post-monsoon seasons. Significant aerosol loading is noticed around ∼2–5.5 km and clean environment below ∼2 km during monsoon. The contribution of aerosols above (below) the boundary layer during monsoon (winter) is found to be around 80% to the total AOD. Back trajectory analyses confirms the advection of aerosols from other land and oceanic regions to the observation site.