Tropospheric ozone variability in Delhi during pre & post monsoon periods: Decoding influence of seasonal variation, diurnal variation, short-range and long-range transport

被引:11
作者
Dhawan, Sachin [1 ]
George, Mohan P. [2 ]
Jayachandran, K. S. [2 ]
Khare, Mukesh [1 ]
机构
[1] Indian Inst Technol, Dept Civil Engn, Delhi 110016, India
[2] Delhi Pollut Control Comm, Delhi 110006, India
关键词
Tropospheric ozone; HYSPLIT back trajectory analysis; Long-range transport; Short-range transport; Meteorological parameters; WEEKDAY-WEEKEND DIFFERENCES; SURFACE OZONE; URBAN SITE; SOURCE APPORTIONMENT; AIR-POLLUTION; IN-SITU; INDIA; PRECURSORS; POLLUTANTS; CHEMISTRY;
D O I
10.1016/j.uclim.2022.101374
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study examines the contribution of various monitoring sites of Delhi categorized as Green Areas, Urban Areas, Industrial/Commercial Areas, Traffic Areas, and Residential Areas. The mean hourly surface O3 concentration during the pre-monsoon season (March - June 2018) varies from 26 +/- 30 to 85 +/- 69 mu g/m3 and in post-monsoon season (October 2018 - January 2019) varies from 13 +/- 18 to 49 +/- 58 mu g/m3. Maximum O3 concentration is found at sites categorized as Green Areas and minimum at Industrial/Commercial Areas for both the pre-and post-monsoon seasons. The contribution of O3 from short-and long-range transport, downward draft, biogenic emissions are found to be maximum at green Areas which act as a sink for the O3. HYSPLIT cluster analysis was done to see the influence of long-range transport on the O3 concentration across all sites. The air masses originating from 3500 m or above contributed more to O3 in green Areas only. Air masses originating from S-W during pre-monsoon and East during post-monsoon contributed to high concentration events in industrial/commercial Areas only. The stubble burning episode in N-W contributed to high concentration events in urban areas and residential areas. The contri-bution of O3 in Residential Areas can be attributed to long-range transport from the N-W di-rection with air-masses originating at height < 1500 m and the local influences.
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页数:16
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