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Simultaneous measurements of surface ozone at two sites over the southern Asia: A comparative study

  • B. Suresh Kumar Reddy
  • , L. S.S. Reddy
  • , Jun Ji Cao
  • , K. Raghavendra Kumar
  • , G. Balakrishnaiah
  • , K. Rama Gopal
  • , R. R. Reddy
  • , K. Narasimhulu
  • , Shyam Lal
  • , Y. Nazeer Ahammed
  • Sri Krishnadevaraya University India
  • CAS - Institute of Earth Environment
  • Government First Grade College
  • Physical Research Laboratory India
  • Yogi Vemana University

Research output: Contribution to journalArticlepeer-review

23 Scopus citations

Abstract

This article presents variations of simultaneous measurements of near surface ozone (O 3) at two sites namely Anantapur [14.62°N, 77.65°E], a semi arid rural location in India and Xi'An [34.20°N, 108.98°E], a semi arid urban location in China during January-July 2009. The results showed a clear diurnal cycle of O 3 with a minimum at sunrise and a maximum at noon for both the sites. The monthly average diurnal variation shows that the maximum/minimum ozone was observed in March/July whereas in Xi'An maximum/minimum ozone was observed in July/February because of different climatic zones and rainfall activity. The average diurnal variation of O3 for different seasons (summer and winter) shows higher ozone concentration at Anantapur than at Xi'An. This may be due to slower titration of NO in the evening hours at Anantapur. But in Xi'An, the highest ozone levels recorded in noon hours for some days in June and July months. This is mainly due to strong emissions of NO x, VOC and high solar radiation and this implies significant negative effects on vegetation and regional air quality around Xi'An. The rate of increase of ozone is almost the same at two sites but the rate of decrease of ozone is more at Xi'An than at Anantapur which is due to the higher NO x concentration from vehicular emission and also due to the fast titration of O 3. The maximum 54% of frequency distribution of ozone lies between 20-45 ppbv at Anantapur whereas in Xi'An 34% lies in the range of 0-5 ppbv, 32% of Ozone lie between 5-20 ppbv and 24% of all O 3 lie in the range of 20-45 ppbv.

Original languageEnglish
Pages (from-to)895-902
Number of pages8
JournalAerosol and Air Quality Research
Volume11
Issue number7
DOIs
StatePublished - Dec 2011

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 11 - Sustainable Cities and Communities
    SDG 11 Sustainable Cities and Communities

Keywords

  • Asian winter monsoon
  • NO
  • Photoxidation
  • Surface ozone

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