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R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering
            Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com
                   Vol. 3, Issue 1, January -February 2013, pp.1527-1531
  Assessment Of Surface Ozone Levels in A Semi-Urban Site and
             Its Predictions Using Neural Network.
                R.Krishna Sharma, T.Chithambarathanu and K.Elampari
               Research Department of Physics, S.T.Hindu College, Nagercoil TamilNadu, India, 629002.


Abstract
         Ozone (O3) is one of the important trace       Considered as an indicator of the overall burden of
gases because of its role as both an oxidant and a      the atmospheric pollutants [3]. Elevated levels of
greenhouse gas. Around 90% of the ozone lies in         surface ozone can cause potential damage to human
the stratosphere and the remaining lies in the          respiratory system and can affect the cilia membrane
Earth’s surface (troposphere).Elevated levels of        of the lungs. Also it can cause damages to
surface ozone can be phytotoxic and cytotoxic as        vegetation and materials as well.
well. This steady intends to access the amount of                 It is now clearly established that ozone, at
surface ozone concentration at a site in                the ambient concentrations can cause a range of ill
Suchindrum (8° 9′ 18″ N, 77° 27′ 54″ E) of              effects including visible leaf injury, growth and
southern Tamilnadu during March 2011-                   yield reductions, and altered sensitivity to biotic and
Febraury 2012 for a period of 12 months. The            abiotic stresses [4]. It is evident that the amount of
surface ozone variation marked a clear diurnal          stratospheric ozone is decreasing while the amount
cycle with maximum values around 1430 hrs and           of tropospheric ozone is increasing. Atmospheric
minimum around 0530 hrs. The maximum value              CO2 concentrations are currently rising at
of surface ozone recorded was 56 ppb during             approximately 0.5% per year and surface ozone
April 2011 and minimum of 13 ppb during                 (ground-level O3) values are increasing at a rate of
November 2011.Seasonal pattern of surface               0.32% per year [5]. So increasing levels of surface
ozone showed maximum values during summer               ozone is really a potential threat to the planet earth.
and minimum during NE Monsoon. Also a                   In order to provide adequate early warnings, it is
simple Neural Network model was proposed to             important to have accurate and reliable forecasts of
predict the peak surface ozone concentration            future high ozone levels [6]. There are many
(1430 hrs) depending upon the various input             different numerical methods for forecasting and
parameters like temperature, relative humidity,         analysing ozone levels and the widely used
Nitrogen      dioxide    and     build-up    ozone      technique is using neural networks. Neural networks
concentration and all corresponding to the              have been found to outperform other statistical
morning hours. The network yields good                  techniques [7]. In this study, a simple neural
predictions and it showed a correlation of r =          network model has been proposed to predict the
0.80 between observed and predicted surface             peak time surface ozone concentration with some of
ozone levels.                                           the important input parameters at Suchindrum
                                                        during the period of March 2011-Febraury 2012.
Key-words: Surface ozone, cytotoxic, diurnal
cycle, seasonal pattern, greenhouse gas, neural         Photo Chemistry of Surface Ozone
network                                                          Surface ozone is not emitted directly into
                                                        the atmosphere. It is produced as the result of
Introduction                                            photochemical reactions between oxides of nitrogen
         The World Health Organisation (WHO)            (NOx) and Volatile organic compounds (VOCs) in
reports that 25% of all preventable diseases are due    the presence of sunlight. During daylight hours
to a poor physical environment. Industrialization,      nitrogen dioxide (NO2) is photolytically converted
population growth and rapid developments in             to nitric oxide (NO) leading to the formation of
technology have all resulted in enormous human          ozone.
impact on the environment [1]. Surface ozone (O3)       NO2 + h ( <= 430nm)  NO + O              (1)
is an important well known secondary pollutant and
also a greenhouse gas contributing to the climate         O + O2  O3                    (2)
change. Even though it is a trace constituent, ozone
plays an important role in the atmospheric                       Therefore, surface ozone control is
environment through radiative and chemical process      generally achieved by reducing the anthropogenic
[2]. O3, being a greenhouse gas, the increase in its    emissions of both NOx and VOCs into the
tropospheric concentration contribute significantly     atmosphere [8].
to local and global warming effects. Ozone is the
primary constituent of photo-oxidative smog and is


                                                                                               1527 | P a g e
R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering
          Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com
                 Vol. 3, Issue 1, January -February 2013, pp.1527-1531
Methods
          Surface ozone measurements were carried
out by using a portable sensitive gaseous monitor
Aeroqual S300 coupled with ozone sensor. Its ultra
low concentration ozone sensor head measures the
ozone concentration from 0.000 to 0.150 ppm with
an accuracy of ± 0.001 ppm (from 0 to 0.100 ppm).
The measurement unit being either ppm or µg/m 3.
The operating temperature range is from - 5°C to
50°C, relative humidity limits are 5% and 95%. The
ozone sensor was calibrated against a certified UV
photometer. Eight readings were taken per day
starting from 0530 h to 0230 h.


                                                            Fig.2. Study Area, Suchindrum

                                                            Results and Discussion
                                                            1. Variation of Surface ozone
                                                                     Surface ozone variations showed a clear
                                                            global diurnal pattern for both the sites. The ozone
                                                            concentration gradually increased after sunrise
                                                            because the photochemical reactions are dominant
                                                            only in the presence of sunlight. The maximum
                                                            value of surface ozone was recorded around 1430 h
                                                            and this is due to the high intensity of solar flux
                                                            during afternoon hours. This indicates that the
 Fig.1. Aeroqual S300 monitor with various sensors          photochemical production of surface ozone is
                                                            strongly related to the surface temperature. During
Study Area                                                  the late evening hours, a decreasing trend was
          Surface ozone measurements were carried           observed in the surface ozone levels. Also this low
out in Suchindrum (8° 918″ N, 77° 27′54″ E) in              concentration of ozone during night and early
Kanyakumari district for a period of one year from          morning time could be a result of its deposition and
March 2011- February 2012.Suchindrum is one of              surface chemical reactions [9]. The morning (0530h)
the tourist spots and traffic prones of the district.       lowest values are the result of night time ozone
                                                            destruction process including loss due to
                                                            atmospheric chemistry and dry deposition on the
                                                            earth.
                                                                     The high values of surface ozone were
                                                            recorded during the months of summer (March –
                                                            May).During the summer, high insulation, high
                                                            temperature; high stability and low mid-day
                                                            humidity produce photochemical smog [10]. The
                                                            lower values were recorded during north east
                                                            monsoon (October to December). Table 1. gives the
                                                            seasonal average values of surface ozone
                                                            concentration and Fig.3 shows its seasonal variation.


Table 1. Seasonal Average of Surface Ozone

Season/Time     5:30        8:30        11:30       14:30       17:30       20:30       23:30       2:30
SUMMER          19.04       26.29       42.43       50.83       44.96       37.87       31.94       24.40
SWM             16.99       22.26       35.98       45.68       40.59       34.21       27.52       21.85
NEM             15.26       19.18       31.29       40.63       34.90       27.62       22.54       18.21
WINTER          19.03       23.39       36.95       46.08       41.53       33.60       27.03       22.35




                                                                                                1528 | P a g e
R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering
               Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com
                      Vol. 3, Issue 1, January -February 2013, pp.1527-1531




               Fig.3. Seasonal variation of Surface ozone during Mar 2011-Feb 2012.
  The overall diurnal average values of surface ozone         parameters for the entire study period are shown in
  concentration     with    various     meteorological        table 2 and figure 4 presents it graphically.

                                           Table 2. Diurnal Average of Surface Ozone

Parameters/time       5:30         8:30          11:30      14:30       17:30        20:30        23:30        2:30
Temperature           25.36        27.21         29.69      30.12       29.02        27.79        27.18        26.21
Ozone                 17.41        22.69         36.58      45.77       40.41        33.37        27.30        21.66
RH                    85.20        76.77         66.49      64.98       70.28        77.01        81.07        82.75
NO2                   4.88         5.31          4.02       1.69        3.85         5.19         6.44         5.12




                  Fig.4. Diurnal variation of Surface ozone with met. Parameters during Mar 2011-Feb 2012.

  2. Network model
           Surface ozone concentration reaches a peak         readings recorded at 0830 hrs and totally the data
  value around 1430 hrs due to the availability               contain 109 sample points.
  dominant solar flux during afternoon hours. The                       The data set is randomly divided into three
  peak value determines whether the particular day is         sets namely training, validation, testing. Training set
  ozone high day or not. So it is very important to           is the largest set (70%) and the remaining sets are
  forecast the peak hour ozone concentration. In this         assigned to contain 15 % of the samples. The
  model, the maximum ozone or peak ozone is                   training set is a set of samples used to adjust or train
  forecasted by using the input parameters like               the weights in the neural network to produce desired
  temperature (T), relative humidity (RH), NO2 and            outcome. The validation set is used to find the best
  surface ozone (O3) itself. These inputs are the data        network configuration and testing set is to evaluate
  corresponding to the morning hours. They are the            the fully trained networks. Eventhough there are

                                                                                                    1529 | P a g e
R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering
            Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com
                   Vol. 3, Issue 1, January -February 2013, pp.1527-1531
many computational functions, the most used             using three neurons in the hidden layer. The model
function in air quality modelling is the sigmoid        is carried out in matlab using Levenberg Marquadrt
function [10]. The Log Sigmoid function is given as     algorithm. The model is presented in the Figure 5.
f(x) = 1/(1+e-x). The model is developed using feed-
forward back propogation multilayer perceptron




                                        Fig.5. Neural Network Model

Model Results
The neural network model is trained using all the
input parameters.The model gives an R2 of 0.85727
for all the data points with MSE of 6.476. Figure 6
shows the scatter plot between the observed and
predicted parameters.




                                                        Fig.7 Observed vs predicted surface ozone levels
Fig 6.Scatter plot between observed and predicted
ozone levels.                                           Conclusion
The correlation between the predicted and the                     Surface ozone measurements were made
observed surface ozone concentration lies around        for a period of one year and the data was analysed
0.8 and the Figure 7 depicts the observed and           with various meteorological parameters. It showed a
predicted levels.                                       well diurnal pattern. The seasonal variation of
                                                        surface ozone showed maximum in summer and
                                                        minimum in NE Monsoon. The data points varied
                                                        between 13 ppb and 56 ppb. A simple neural
                                                        network model was designed to predict the peak
                                                        hour ozone concentration and it yielded good
                                                        correlation between observed and predicted ozone

                                                                                           1530 | P a g e
R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering
            Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com
                   Vol. 3, Issue 1, January -February 2013, pp.1527-1531
levels. Even though the ozone levels are within the
permissible air quality standards of 60 ppb,
continuous monitoring is essential.

References
  [1]    Rasa Girgzdiene, Aloyzas Girgzdys, The
         Troposphere Ozone – an Indicator of the
         Environmental Sustainability, Journal of
         Environmental research, engineering and
         management, Vol.26,No.4,2003,pp.45-50.
  [2]    A.L. Londhe, D. J.           Surface ozone
         variability in the urban and nearby rural
         locations of tropical India. CURRENT
         SCIENCE, VOL. 95, NO. 12.2008.
  [3]    Elampari K, Chithambarathanu T, Krishna
         Sharma R, Examining the variations of
         ground level ozone and nitrogen dioxide in
         a rural area influenced by brick kiln
         industries, Indian journal of Science and
         technology,Vol.3,No.8,2010.
  [4]    Grunhage L, Jager HJ, Influence of the
         atmospheric conductivity on the ozone
         exposure of plants under ambient
         conditions,     Environmental      pollution,
         Vol.85, No.2, 1994, pp.125-129.
  [5]    Akram Ali, Factors Affecting on Response
         of Broad Bean and Corn to Air Quality and
         Soil CO2 Flux rates in Egypt, Journal of
         water, air and soil pollution,Vol.195,No.1-
         4,2008,pp.311-323.
  [6]    Dominik Wieland and Franz Otawa,Local
         Maximum ozone concentration prediction
         using neural networks,AAAI Technical
         Report ,1999 WS 99-07.
  [7]    Arigiriou.A, Use of neural networks for
         tropospheric      ozone      time      series
         approximation        and        forecasting,a
         review.,Atmos.Chem.Phys-Discuss.           7,
         2007, pp.5739-5767.
  [8]    Lin Tang, Regional and local surface ozone
         variations in relation to meteorological
         conditions in Sweden, Ph.D.,Thesis,
         Department of Earth Sciences, University
         of Gothenburg, Sweden, 2009.
  [9]    S. Renuka GS, Satsangi and Taneja A,
         Concentrations of surface O3, NO2 and CO
         during winter seasons at a semi-arid region
         Agra, India, Indian Journal of Radio &
         Space Physics, vol.37, 2008,pp. 121-130.
  [10]   Seinfeld.J.H.,    Pandis,S.N.,From        Air
         pollution to climate change, Atmospheric
         chemistry                                 and
         Physics,1998,J.wiley,Newyork.




                                                                             1531 | P a g e

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  • 1. R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com Vol. 3, Issue 1, January -February 2013, pp.1527-1531 Assessment Of Surface Ozone Levels in A Semi-Urban Site and Its Predictions Using Neural Network. R.Krishna Sharma, T.Chithambarathanu and K.Elampari Research Department of Physics, S.T.Hindu College, Nagercoil TamilNadu, India, 629002. Abstract Ozone (O3) is one of the important trace Considered as an indicator of the overall burden of gases because of its role as both an oxidant and a the atmospheric pollutants [3]. Elevated levels of greenhouse gas. Around 90% of the ozone lies in surface ozone can cause potential damage to human the stratosphere and the remaining lies in the respiratory system and can affect the cilia membrane Earth’s surface (troposphere).Elevated levels of of the lungs. Also it can cause damages to surface ozone can be phytotoxic and cytotoxic as vegetation and materials as well. well. This steady intends to access the amount of It is now clearly established that ozone, at surface ozone concentration at a site in the ambient concentrations can cause a range of ill Suchindrum (8° 9′ 18″ N, 77° 27′ 54″ E) of effects including visible leaf injury, growth and southern Tamilnadu during March 2011- yield reductions, and altered sensitivity to biotic and Febraury 2012 for a period of 12 months. The abiotic stresses [4]. It is evident that the amount of surface ozone variation marked a clear diurnal stratospheric ozone is decreasing while the amount cycle with maximum values around 1430 hrs and of tropospheric ozone is increasing. Atmospheric minimum around 0530 hrs. The maximum value CO2 concentrations are currently rising at of surface ozone recorded was 56 ppb during approximately 0.5% per year and surface ozone April 2011 and minimum of 13 ppb during (ground-level O3) values are increasing at a rate of November 2011.Seasonal pattern of surface 0.32% per year [5]. So increasing levels of surface ozone showed maximum values during summer ozone is really a potential threat to the planet earth. and minimum during NE Monsoon. Also a In order to provide adequate early warnings, it is simple Neural Network model was proposed to important to have accurate and reliable forecasts of predict the peak surface ozone concentration future high ozone levels [6]. There are many (1430 hrs) depending upon the various input different numerical methods for forecasting and parameters like temperature, relative humidity, analysing ozone levels and the widely used Nitrogen dioxide and build-up ozone technique is using neural networks. Neural networks concentration and all corresponding to the have been found to outperform other statistical morning hours. The network yields good techniques [7]. In this study, a simple neural predictions and it showed a correlation of r = network model has been proposed to predict the 0.80 between observed and predicted surface peak time surface ozone concentration with some of ozone levels. the important input parameters at Suchindrum during the period of March 2011-Febraury 2012. Key-words: Surface ozone, cytotoxic, diurnal cycle, seasonal pattern, greenhouse gas, neural Photo Chemistry of Surface Ozone network Surface ozone is not emitted directly into the atmosphere. It is produced as the result of Introduction photochemical reactions between oxides of nitrogen The World Health Organisation (WHO) (NOx) and Volatile organic compounds (VOCs) in reports that 25% of all preventable diseases are due the presence of sunlight. During daylight hours to a poor physical environment. Industrialization, nitrogen dioxide (NO2) is photolytically converted population growth and rapid developments in to nitric oxide (NO) leading to the formation of technology have all resulted in enormous human ozone. impact on the environment [1]. Surface ozone (O3) NO2 + h ( <= 430nm)  NO + O (1) is an important well known secondary pollutant and also a greenhouse gas contributing to the climate O + O2  O3 (2) change. Even though it is a trace constituent, ozone plays an important role in the atmospheric Therefore, surface ozone control is environment through radiative and chemical process generally achieved by reducing the anthropogenic [2]. O3, being a greenhouse gas, the increase in its emissions of both NOx and VOCs into the tropospheric concentration contribute significantly atmosphere [8]. to local and global warming effects. Ozone is the primary constituent of photo-oxidative smog and is 1527 | P a g e
  • 2. R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com Vol. 3, Issue 1, January -February 2013, pp.1527-1531 Methods Surface ozone measurements were carried out by using a portable sensitive gaseous monitor Aeroqual S300 coupled with ozone sensor. Its ultra low concentration ozone sensor head measures the ozone concentration from 0.000 to 0.150 ppm with an accuracy of ± 0.001 ppm (from 0 to 0.100 ppm). The measurement unit being either ppm or µg/m 3. The operating temperature range is from - 5°C to 50°C, relative humidity limits are 5% and 95%. The ozone sensor was calibrated against a certified UV photometer. Eight readings were taken per day starting from 0530 h to 0230 h. Fig.2. Study Area, Suchindrum Results and Discussion 1. Variation of Surface ozone Surface ozone variations showed a clear global diurnal pattern for both the sites. The ozone concentration gradually increased after sunrise because the photochemical reactions are dominant only in the presence of sunlight. The maximum value of surface ozone was recorded around 1430 h and this is due to the high intensity of solar flux during afternoon hours. This indicates that the Fig.1. Aeroqual S300 monitor with various sensors photochemical production of surface ozone is strongly related to the surface temperature. During Study Area the late evening hours, a decreasing trend was Surface ozone measurements were carried observed in the surface ozone levels. Also this low out in Suchindrum (8° 918″ N, 77° 27′54″ E) in concentration of ozone during night and early Kanyakumari district for a period of one year from morning time could be a result of its deposition and March 2011- February 2012.Suchindrum is one of surface chemical reactions [9]. The morning (0530h) the tourist spots and traffic prones of the district. lowest values are the result of night time ozone destruction process including loss due to atmospheric chemistry and dry deposition on the earth. The high values of surface ozone were recorded during the months of summer (March – May).During the summer, high insulation, high temperature; high stability and low mid-day humidity produce photochemical smog [10]. The lower values were recorded during north east monsoon (October to December). Table 1. gives the seasonal average values of surface ozone concentration and Fig.3 shows its seasonal variation. Table 1. Seasonal Average of Surface Ozone Season/Time 5:30 8:30 11:30 14:30 17:30 20:30 23:30 2:30 SUMMER 19.04 26.29 42.43 50.83 44.96 37.87 31.94 24.40 SWM 16.99 22.26 35.98 45.68 40.59 34.21 27.52 21.85 NEM 15.26 19.18 31.29 40.63 34.90 27.62 22.54 18.21 WINTER 19.03 23.39 36.95 46.08 41.53 33.60 27.03 22.35 1528 | P a g e
  • 3. R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com Vol. 3, Issue 1, January -February 2013, pp.1527-1531 Fig.3. Seasonal variation of Surface ozone during Mar 2011-Feb 2012. The overall diurnal average values of surface ozone parameters for the entire study period are shown in concentration with various meteorological table 2 and figure 4 presents it graphically. Table 2. Diurnal Average of Surface Ozone Parameters/time 5:30 8:30 11:30 14:30 17:30 20:30 23:30 2:30 Temperature 25.36 27.21 29.69 30.12 29.02 27.79 27.18 26.21 Ozone 17.41 22.69 36.58 45.77 40.41 33.37 27.30 21.66 RH 85.20 76.77 66.49 64.98 70.28 77.01 81.07 82.75 NO2 4.88 5.31 4.02 1.69 3.85 5.19 6.44 5.12 Fig.4. Diurnal variation of Surface ozone with met. Parameters during Mar 2011-Feb 2012. 2. Network model Surface ozone concentration reaches a peak readings recorded at 0830 hrs and totally the data value around 1430 hrs due to the availability contain 109 sample points. dominant solar flux during afternoon hours. The The data set is randomly divided into three peak value determines whether the particular day is sets namely training, validation, testing. Training set ozone high day or not. So it is very important to is the largest set (70%) and the remaining sets are forecast the peak hour ozone concentration. In this assigned to contain 15 % of the samples. The model, the maximum ozone or peak ozone is training set is a set of samples used to adjust or train forecasted by using the input parameters like the weights in the neural network to produce desired temperature (T), relative humidity (RH), NO2 and outcome. The validation set is used to find the best surface ozone (O3) itself. These inputs are the data network configuration and testing set is to evaluate corresponding to the morning hours. They are the the fully trained networks. Eventhough there are 1529 | P a g e
  • 4. R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com Vol. 3, Issue 1, January -February 2013, pp.1527-1531 many computational functions, the most used using three neurons in the hidden layer. The model function in air quality modelling is the sigmoid is carried out in matlab using Levenberg Marquadrt function [10]. The Log Sigmoid function is given as algorithm. The model is presented in the Figure 5. f(x) = 1/(1+e-x). The model is developed using feed- forward back propogation multilayer perceptron Fig.5. Neural Network Model Model Results The neural network model is trained using all the input parameters.The model gives an R2 of 0.85727 for all the data points with MSE of 6.476. Figure 6 shows the scatter plot between the observed and predicted parameters. Fig.7 Observed vs predicted surface ozone levels Fig 6.Scatter plot between observed and predicted ozone levels. Conclusion The correlation between the predicted and the Surface ozone measurements were made observed surface ozone concentration lies around for a period of one year and the data was analysed 0.8 and the Figure 7 depicts the observed and with various meteorological parameters. It showed a predicted levels. well diurnal pattern. The seasonal variation of surface ozone showed maximum in summer and minimum in NE Monsoon. The data points varied between 13 ppb and 56 ppb. A simple neural network model was designed to predict the peak hour ozone concentration and it yielded good correlation between observed and predicted ozone 1530 | P a g e
  • 5. R.Krishna Sharma, Chithambarathanu, K.Elampari / International Journal of Engineering Research and Applications (IJERA) ISSN: 2248-9622 www.ijera.com Vol. 3, Issue 1, January -February 2013, pp.1527-1531 levels. Even though the ozone levels are within the permissible air quality standards of 60 ppb, continuous monitoring is essential. References [1] Rasa Girgzdiene, Aloyzas Girgzdys, The Troposphere Ozone – an Indicator of the Environmental Sustainability, Journal of Environmental research, engineering and management, Vol.26,No.4,2003,pp.45-50. [2] A.L. Londhe, D. J. Surface ozone variability in the urban and nearby rural locations of tropical India. CURRENT SCIENCE, VOL. 95, NO. 12.2008. [3] Elampari K, Chithambarathanu T, Krishna Sharma R, Examining the variations of ground level ozone and nitrogen dioxide in a rural area influenced by brick kiln industries, Indian journal of Science and technology,Vol.3,No.8,2010. [4] Grunhage L, Jager HJ, Influence of the atmospheric conductivity on the ozone exposure of plants under ambient conditions, Environmental pollution, Vol.85, No.2, 1994, pp.125-129. [5] Akram Ali, Factors Affecting on Response of Broad Bean and Corn to Air Quality and Soil CO2 Flux rates in Egypt, Journal of water, air and soil pollution,Vol.195,No.1- 4,2008,pp.311-323. [6] Dominik Wieland and Franz Otawa,Local Maximum ozone concentration prediction using neural networks,AAAI Technical Report ,1999 WS 99-07. [7] Arigiriou.A, Use of neural networks for tropospheric ozone time series approximation and forecasting,a review.,Atmos.Chem.Phys-Discuss. 7, 2007, pp.5739-5767. [8] Lin Tang, Regional and local surface ozone variations in relation to meteorological conditions in Sweden, Ph.D.,Thesis, Department of Earth Sciences, University of Gothenburg, Sweden, 2009. [9] S. Renuka GS, Satsangi and Taneja A, Concentrations of surface O3, NO2 and CO during winter seasons at a semi-arid region Agra, India, Indian Journal of Radio & Space Physics, vol.37, 2008,pp. 121-130. [10] Seinfeld.J.H., Pandis,S.N.,From Air pollution to climate change, Atmospheric chemistry and Physics,1998,J.wiley,Newyork. 1531 | P a g e