Surface ozone over Doon valley of the Indian Himalaya: Characteristics, impact assessment, and model results
Source
Atmospheric Environment X
Date Issued
2024-01-01
Author(s)
Harithasree, S.
Sharma, Kiran
Girach, Imran A.
Sahu, Lokesh K.
Nair, Prabha R.
Singh, Narendra
Flemming, Johannes
Babu, S. Suresh
Ojha, N.
Abstract
The air quality and climate of the Himalaya is found to be impacted profoundly by strong anthropogenic emissions and photochemical processes in the valley region. Considering rapid urbanization and population growth, we performed surface ozone (O<inf>3</inf>) measurements over Doon valley of the Indian Himalaya during April 2018–June 2023, in conjunction with the analysis of satellite observations and modeling. Noontime O<inf>3</inf> levels are observed to be the highest during pre-monsoon (63.8 ± 15.3 ppbv in May) and lower (22.1–56.7 ppbv) during winter and monsoon seasons. Notably, the daily maximum 8-h average (MDA8) O<inf>3</inf> exceeds the 50 ppbv threshold for ∼60% of the days during April–June, which suggests substantial health impacts in the region. Impact of O<inf>3</inf> exposure on vegetation is also significant during this period of year, as reflected from high Accumulated Ozone above Threshold 40 ppbv (AOT40) and Mean of daytime 7 hours (M7) indices. The Copernicus Atmosphere Monitoring Service (CAMS) reanalysis successfully reproduced the observed variability in the noontime O<inf>3</inf> (r<sup>2</sup> = 0.79–0.91). Analysis of a tracer in the CAMS model shows that the mean stratospheric contributions to surface O<inf>3</inf> were typically smaller (up to 8%). This suggests that O<inf>3</inf> pollution is governed primarily by the photochemical production favored by regional emissions and meteorological conditions. Analysis combining in-situ O<inf>3</inf> measurements with satellite retrievals (HCHO and NO<inf>2</inf>) revealed that the photochemical O<inf>3</inf> production is in the transition or VOC-limited regime, and therefore emission of both NO<inf>x</inf> and volatile organic compounds (VOCs) are to be reduced to mitigate O<inf>3</inf> pollution. Finally, a statistical model considering the non-linearities was successfully applied to simulate observed O<inf>3</inf> variability from available satellite observations and meteorological reanalysis data (r<sup>2</sup> = 0.75, RMSE = 7 ppbv). Our study highlights the need to mitigate O<inf>3</inf> pollution in the Doon valley of the Indian Himalaya and also provides invaluable inputs for designing science-informed policies.
Subjects
Air quality | CAMS reanalysis | Chemical regime | Crop yield | MDA8 | Ozone pollution | Photochemistry | Statistical modeling | Trace gases | TROPOMI
