Kumar A Hemanth, Ratnam M Venkat, Jain Chaithanya D
National Atmospheric Research Laboratory (NARL), Gadanki 517112, India.
Atmos Res. 2022 Jan;265:105876. doi: 10.1016/j.atmosres.2021.105876. Epub 2021 Oct 5.
The COVID-19 pandemic lockdown has led to the significant reductions in the pollutant levels across the globe. Several studies have been carried out for examining and quantifying the improvement in the air quality due to the reduction of the pollution at the surface. Unlike most of the studies carried out earlier on COVID-19 lockdown, this study investigates the role of the dynamics on the vertical distribution of the trace gases (Carbonmonoxide (CO), Water Vapor (WV) and Ozone (O)) over India in the Boundary Layer (BL), Middle Troposphere (MT) and Upper Troposphere (UT) during COVID-19 lockdown using satellite observations and re-analysis data products obtained during 2010-2020. Substantial differences in the time series and variability have been observed over different zones of India in different atmospheric layers. The changes observed in these species are large over Central India compared to South India and Indo-Gangetic plain regions. An enhancement in CO (~25-40%) and WV (50-60%) has been noticed over Central India in the UT at 147 hPa and 215 hPa, respectively, during lockdown. The strong updrafts before the lockdown and the extended weak zonal wind aloft over this region are found responsible for the observed enhancement in these trace gases in the UT. In spite of the non-availability of the anthropogenic pollution during the lockdown, this study highlights the transport of pollutants through long-range transport (always present even before lockdown) dominance over the Indian region not only near the surface but also aloft due to associated atmospheric dynamics.
新冠疫情封锁导致全球污染物水平大幅下降。已经开展了多项研究,以检查和量化由于地表污染减少而带来的空气质量改善情况。与之前关于新冠疫情封锁的大多数研究不同,本研究利用2010 - 2020年期间获得的卫星观测和再分析数据产品,调查了新冠疫情封锁期间印度边界层(BL)、对流层中层(MT)和对流层上层(UT)中痕量气体(一氧化碳(CO)、水汽(WV)和臭氧(O))垂直分布的动力学作用。在印度不同区域的不同大气层中,观测到时间序列和变率存在显著差异。与印度南部和印度 - 恒河平原地区相比,印度中部这些物种的变化更大。在封锁期间,分别在147百帕和215百帕的对流层上层,印度中部的一氧化碳(约25 - 40%)和水汽(50 - 60%)有所增加。该地区封锁前的强烈上升气流以及高空长时间存在的弱纬向风被认为是对流层上层这些痕量气体增加的原因。尽管封锁期间没有人为污染,但本研究强调,由于相关的大气动力学,污染物不仅在地表附近,而且在高空通过长距离传输(即使在封锁前也一直存在)在印度地区占主导地位。