CSIR-National Physical Laboratory, Dr. K.S. Krishnan Marg, New Delhi 110012, India; Academy of Scientific and Innovative Research (AcSIR), Ghaziabad 201002, India.
CSIR-National Physical Laboratory, Dr. K.S. Krishnan Marg, New Delhi 110012, India; Academy of Scientific and Innovative Research (AcSIR), Ghaziabad 201002, India.
Sci Total Environ. 2022 Feb 1;806(Pt 1):150127. doi: 10.1016/j.scitotenv.2021.150127. Epub 2021 Sep 5.
The four-year continuous measurements of CO, NOx, NH, SO and O were carried at a high altitude site (32.12°N, 76.56°E at 1347 m AMSL) of the Indian Western Himalayan area to study the mixing ratios of these gases for understanding the changing trends of these trace gases over the region. Each of these trace gases showed significant daily and monthly variabilities. The highest variability was recorded in the monthly mean values of O as it varied from 10 to 63 ppb during the study period. All the trace gases except CO showed maximum variability in the pre-monsoon seasons due to the strong advection and vertical circulation of air masses at the site. The seasonal mean maxima of CO were recorded during the monsoon season, while the mean maxima of NH were recorded during the post-monsoon seasons. The meteorological parameters have been found to influence the mixing ratios of trace gases. The least variability in the mean seasonal mixing ratios of SO during the study period indicated the constant point source of SO near the site. The trajectories analysis revealed that the area receives maximum air masses from the southeast to the west directions where a number of the coal-based thermal power plants, industries, cement plants, and agricultural fields are also located. The influence of valley-to-mountain circulations was also observed at the site, resulting in the transport of pollutant-rich air masses from local and distant sources to the site. A comparison of the mixing ratios of different trace gases obtained in the present study is also made with the values reported for other high altitude stations in the world.
在印度喜马拉雅西部地区的一个高海拔站点(32.12°N,76.56°E,海拔 1347 米)进行了为期四年的 CO、NOx、NH、SO 和 O 的连续测量,以研究这些气体的混合比,以了解该地区这些痕量气体的变化趋势。这些痕量气体中的每一种都表现出明显的日变化和月变化。O 的月均值变化最大,在研究期间,其变化范围从 10 到 63 ppb。除 CO 外,所有痕量气体在季风前季节的变化最大,这是由于该站点的空气团强烈平流和垂直环流造成的。CO 的季节均值最大值出现在季风季节,而 NH 的季节均值最大值出现在季风后季节。气象参数被发现对痕量气体的混合比有影响。SO 的平均季节混合比在研究期间变化最小,表明该站点附近存在稳定的 SO 点源。轨迹分析显示,该地区从东南向西北方向接收最大的空气团,其中有许多燃煤热电厂、工业、水泥厂和农田。该站点还观察到山谷到山地的环流的影响,导致来自当地和遥远源的富含污染物的空气团输送到该站点。还将本研究中获得的不同痕量气体的混合比与世界其他高海拔站点报告的值进行了比较。