Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia

Hourly ground ozone concentration, measured from the monitoring stations in the West Coast of Peninsular Malaysia for the period of 10 years (2003-2012) were used to analyse the ozone characteristic in Nilai, Melaka and Petaling Jaya. The prediction of tropospheric ozone concentrations is very impor...

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Main Authors: Hashim Nur Izzah Mohamad, Noor Norazian Mohamed
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:MATEC Web of Conferences
Online Access:https://doi.org/10.1051/matecconf/20179701048
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spelling doaj-0086630f6c8d41d18b549b6f904ba9df2021-02-02T01:39:29ZengEDP SciencesMATEC Web of Conferences2261-236X2017-01-01970104810.1051/matecconf/20179701048matecconf_etic2017_01048Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular MalaysiaHashim Nur Izzah Mohamad0Noor Norazian Mohamed1School of Environmental Engineering, University Malaysia Perlis (UniMAP)School of Environmental Engineering, University Malaysia Perlis (UniMAP)Hourly ground ozone concentration, measured from the monitoring stations in the West Coast of Peninsular Malaysia for the period of 10 years (2003-2012) were used to analyse the ozone characteristic in Nilai, Melaka and Petaling Jaya. The prediction of tropospheric ozone concentrations is very important due to the negative impacts of ozone on human health, climate and vegetation. The mean concentration of ozone at the studied areas had not exceeded the recommended value of Malaysia Ambient Air Quality Guideline (MAAQG) for 8-hour average (0.06 ppm), however some of the measurements exceeded the hourly permitted concentration by MAAQG that is 0.1 ppm. Higher concentration of ozone can be observed during the daytime since ozone needs sunlight for the photochemical reactions. The diurnal cycle of ozone concentration has a mid-day peak (14:00-15:00) and lower night-time concentrations. The ozone concentration slowly rises after the sun rises (08:00), reaching a maximum during daytime and then decreases until the next morning.https://doi.org/10.1051/matecconf/20179701048
collection DOAJ
language English
format Article
sources DOAJ
author Hashim Nur Izzah Mohamad
Noor Norazian Mohamed
spellingShingle Hashim Nur Izzah Mohamad
Noor Norazian Mohamed
Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
MATEC Web of Conferences
author_facet Hashim Nur Izzah Mohamad
Noor Norazian Mohamed
author_sort Hashim Nur Izzah Mohamad
title Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
title_short Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
title_full Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
title_fullStr Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
title_full_unstemmed Variations of Ground-level Ozone Concentration in Malaysia: A Case Study in West Coast of Peninsular Malaysia
title_sort variations of ground-level ozone concentration in malaysia: a case study in west coast of peninsular malaysia
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2017-01-01
description Hourly ground ozone concentration, measured from the monitoring stations in the West Coast of Peninsular Malaysia for the period of 10 years (2003-2012) were used to analyse the ozone characteristic in Nilai, Melaka and Petaling Jaya. The prediction of tropospheric ozone concentrations is very important due to the negative impacts of ozone on human health, climate and vegetation. The mean concentration of ozone at the studied areas had not exceeded the recommended value of Malaysia Ambient Air Quality Guideline (MAAQG) for 8-hour average (0.06 ppm), however some of the measurements exceeded the hourly permitted concentration by MAAQG that is 0.1 ppm. Higher concentration of ozone can be observed during the daytime since ozone needs sunlight for the photochemical reactions. The diurnal cycle of ozone concentration has a mid-day peak (14:00-15:00) and lower night-time concentrations. The ozone concentration slowly rises after the sun rises (08:00), reaching a maximum during daytime and then decreases until the next morning.
url https://doi.org/10.1051/matecconf/20179701048
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