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Daytime Ozone Variation in Surface Air in a Subtropical Mangrove Estuary at Manakudy, South India | ||
Pollution | ||
مقاله 11، دوره 4، شماره 4، دی 2018، صفحه 675-685 اصل مقاله (665.52 K) | ||
نوع مقاله: Original Research Paper | ||
شناسه دیجیتال (DOI): 10.22059/poll.2018.251912.390 | ||
نویسندگان | ||
R. Krishna Sharma* 1؛ T Chithambarathau1؛ K. Elampari1؛ S. Nagaveena2 | ||
1Department of Physics, South Travancore Hindu College, Nagercoil-629002, Tamil Nadu, India | ||
2Department of Physics,KalasalingamUniversity,Krishnankoil, Tamil Nadu, India | ||
چکیده | ||
Surface ozone (SOZ) can be very harmful if it exceeds the threshold limit. It can accumulate over sea and can return back to the land along with the breeze. Rural and vegetation rich areas often record elevated levels of surface ozone because of the variations in Volatile Organic Compound (VOC) levels, wind velocity and direction. Similarly methane is also an important greenhouse gas and plays a vital role in the atmospheric budget. In this work, ozone and methane levels measured during daytime in a mangrove estuary near Manakudy(8.0911 N, 77.477 E),kanyakumari, South India for a period of ten months from March 2014 to December 2014 are analyzed.SOZ showed an imprecise diurnal pattern with an early morning peak whereas methane recorded an apparent diurnality. The maximum value of SOZ was around 50 ppb. Summer months recorded high levels of SOZ followed by Southwest monsoon (SWM) and Northeast monsoon (NEM).High levels of methane were found in SWM followed by NEM and low concentration during summer. The correlation between SOZ and methane was found as r = -0.257, p | ||
کلیدواژهها | ||
VOC؛ estuary؛ diurnal؛ Greenhouse؛ Correlation؛ meteorology | ||
مراجع | ||
Agudelo-Castaneda, D.and Teixeiria, L. (2013). Measurement of Particle Number and Related Pollutant Concentrations in an Urban Area in South Brazil. J. Atmos. Environ., 70;254–262. Anet, J. G., Steinbacher, M., Gallardo, L., VelásquezÁlvarez, P. A., Emmenegger, L. and Buchmann, B. (2017). Surface ozone in the Southern Hemisphere: 20 years of data from a site with a unique setting in El Tololo, Chile,. Atmos. Chem. Phys., 17; 6477-6492. Brühl, C. and Crutzen, P.J. (1989). On the disproportionate role of tropospheric ozone as a filter against solar UV-B radiation. J. Geophys. Res. Lett. 16;703-706. Chandrasekhar R. and Balaji, C. (2012). Sensitivity of tropical cyclone Jal simulations to physics parameterizations,. J. Earth Syst. Sci., 121;923-946. Crutzen, P.J. (1973).A discussion of some minor constituents in the stratosphere and troposphere. J. Pure Appl. Geophys.,1385–1399. Demerjian, K.L., Schere,L. and Peterson, J.T. (1980). Theoretical estimates of actinic (spherically integrated) flux and photolytic rate constants of atmospheric species in the lower troposphere. J. Adv Env. Sci. Technol., 10;369-459. Doherty, R.M., Wild, R. and Shindell, D.T . (2013) Impacts of climate change on surface ozone and intercontinental ozone pollution: A multi-model study. J. Geo. Phy. Res. Atm.,118;3744 – 3763. Widen, D. A. (1966). Concentration of ozone in surface air over greater Boston. Doctoral dissertation, , Massachusetts Institute of Technology. EPA U.S (2003). Office of Air and Radiation ozone: Good up High, Bad nearly – EPA-451/K-03-001. Washington, DC: US Environmental protection Agency. EPA U.S (1999b). Office of Air and Radiation. Smog-who does It Hurt-EPA-452/f-99-001. Washington, DC: US Environmental protection Agency. Fishman, J., Watson, C. E., Larsen, J. C. and Logan, J. A. (1990). Distribution of tropospheric ozone determined from satellite data. J. Geophys. Res., 95;3599-3617. Hsu, K. J. (2007). Relationship between ten-year trends of tropospheric ozone and temperature over Taiwan. Sci. Total Environ., 374;135- 142. Logan, J. A., Prather, M. J., Wofsy, S. and McElroy, M. B. (1981). Tropospheric Chemistry: A global perspective. J. Geophy. Res., 86:7210-7254. McElroy, M. (2002). Effects of Human Activity. The Atmos.Environ.: Princeton University Press, Princeton. Nishanth, T. and Satheesh Kumar, M. K. (2011).Diurnal variation of Surface ozone with meteorological parameters at Kannur, India. Adv. Appl. Sci. Res., 2;407-417. Naja, M. And Lal, S. (2002).Surface ozone and precursor gases at Gadanki (13.5°N, 79.2°E), a tropical rural site in India. J.Geophys. Res.,107(14); 4197. Ohara, T., Akimoto, H., Kurokawa, J., Horii, N., Yamaji, K., Yan X. and Hayasaka, T. (2007). An Asian emission inventory of anthropogenic emission sources for the period 1980–2020. Atmos. Chem. Phys., 7;4419–4444. Panday, A.K. and Prinn, R.G. (2009). Diurnal cycle of air pollution in the Kathmandu Valley, Nepal: observations. J. Geophys. Res.,114;D09305. Pathak, H., Li, C. and Wassmann, R. (2005). Greenhouse gas emissions from Indian rice fields: calibration and up scaling using the DNDC model. Biogeosci., 2;113–123. Peterson, J.T. (1976). Calculated actinic fluxes (290-700 nm) for air pollution photochemistry application.EPA 600/4-76-025. U.S. Environmental Protection Agency. Pugliese, S.C., Murphy, J.G. and Geddes, J.A .(2014). The impacts of precursor reduction and meteorology on ground-level ozone in the Greater Toronto Area. J.Atmos. Chem. Phy., 14; 8197–8207. Rao, Y. P. and Ramamurthy, K. S. (1972).Climatology of India and neighbourhood, forecasting manual. Part I., IMD, Poona -5. Reddy, R.R. and RamaGopal, K. (2008). Measurement of CO and SO2 trace gases in southern India during ISRO - GBP Land campaign - I. Ind. J. Radio Space Phys., 37;216-220. Tyson, P. D., Kruger, F. J. and Louw, C.W. (1988). Atmospheric pollution and its implications in the Eastern Transvaal Highveld, South African National Scientific Programmes Report no.150(4);40. Streets, D. G., Canty, T., Carmichael, G. R., Foy, B., Dickerson, R. R., Duncan, B. N., Edward, D. P., Haynes, J. A., Henze, D. K., Houyoux, M. R., Jacob, D. J., Krotkove, N. A., Lamsal, L. N., Liu,Y. K., Lu, Z., Martin, R.V., Pfister, G. G., Pinder, R. W., Salawitch, R. J. and Wecht, K. J. (2013). Emissions estimation from satellite retrievals: a review of current capability. Atmos Environ., 77; 1011–1042. Walcek, C. J. and Yuan, H. H. (1999).Calculated influence of temperature – related factors on ozone formation rates in the lower troposphere.J. Appl. Meteorol., 34(5);1056-1069. White, A.B. and Templeman, B.D. (2002). Regional contrast in morning transitions observed during the 1999 southern oxidants study Nashville/middle Tennessee intensive. J. Geophy. Res., 107;4726. | ||
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