On the processes influencing the vertical distribution of ozone over the central Himalayas: Analysis of yearlong ozonesonde observations

• Published in: Atmospheric environment (1994) 2014-05, Vol.88, p.201-211
• Main Authors: Ojha, N., Naja, M., Sarangi, T., Kumar, R., Bhardwaj, P., Lal, S., Venkataramani, S., Sagar, R., Kumar, A., Chandola, H.C.
• Format: Article
• Language: English
• Subjects: Biomass-burning; Central Himalayas; Chemical composition and interactions. Ionic interactions and processes; Earth, ocean, space; Exact sciences and technology; External geophysics; Indo-Gangetic Plain; Meteorology; Ozonesonde; Regional pollution; Stratospheric intrusion
• ISSN: 1352-2310; 1873-2844
• DOI: 10.1016/j.atmosenv.2014.01.031

First yearlong (2011) balloon-borne measurements of ozone vertical distribution (EN-SCI 2ZV7 ECC Ozonesonde) and meteorological parameters (iMet-1-RSB 403 MHz GPS Radiosonde) over Nainital (79.5°E, 29.4°N, 1958 m amsl) in the central Himalayas are presented. Lower tropospheric ozone shows a prominent seasonality with highest levels during spring (∼70–110 ppbv in May) and lowest levels during summer-monsoon (∼20–50 ppbv), which is consistent with the ground-based observations. The lower tropospheric ozone minimum coincides with highest values of relative humidity (80–100%) during the summer-monsoon. However, ozone mixing ratios in the middle-upper troposphere show less pronounced and different seasonality. Influences of subtropical jets are observed (wind speed: ∼40–80 m s−1) in the middle-upper troposphere, particularly during winter. A stratospheric intrusion event during winter is observed, which enhances the ozone levels by ∼180% in the middle-upper troposphere. A noticeable feature of secondary ozone peaks (∼140–250 ppbv) is observed in the middle troposphere (∼8–12 km), more frequently during spring. Ozone levels in 2–4 km altitude range are higher by 19.9 ± 4.6 ppbv during the springtime high fire activity period over the northern India. Moreover, the lower tropospheric ozone levels over Nainital during spring are found to be considerably (∼30 ppbv) higher than those over Ahmedabad in the western India. This ozone enhancement is attributed mainly to the regional pollution of the Indo-Gangetic Plain (IGP) supplemented with the northern Indian biomass burning. It is suggested that regional photochemistry and biomass burning processes play controlling role in the lower troposphere, while, the middle-upper tropospheric variations are driven by dynamical processes including advection and stratospheric intrusion. •First yearlong ozonesonde-radiosonde observations over the central Himalayas.•Stratospheric intrusion enhances ozone significantly in middle-upper troposphere.•Influence of northern Indian biomass burning on ozone distribution.•Invaluable data for evaluation of models and satellite products.