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首页> 外文期刊>Pollution >Summer time variation and unexpected nocturnal peak in precursors related Surface ozone concentration in air over a tropical coastal regionof Southern Tamil Nadu, India
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Summer time variation and unexpected nocturnal peak in precursors related Surface ozone concentration in air over a tropical coastal regionof Southern Tamil Nadu, India

机译:印度南部泰米尔纳德邦热带沿海地区空气中与表面臭氧浓度相关的前体的夏季时间变化和意想不到的夜间峰值

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摘要

Surface ozone (Surface O3)is a secondary pollutant and there are only limited studies on ozone in South India. Studies have revealed a strong correlation between higher ozone levels and warmer days. Surface O3 along with its precursors like NO2, CO and CH4 are being measured at Kanyakumari (8.0780° N, 77.5410° E), TamilNadu, India and in this paper we present the summer time variation of ozone from 2010to 2014 . Surface O3 showed a clear diurnal variation, but an irregularity was observed during the night time for all the measuring days of Summer 2014.There was a formation of a well pronounced secondary peak in Surface O3 during 0230 hrs accompanied by relatively strong wind patterns. Since the normal diurnal variation cannot explain this phenomenon,this uncertain behavior is probably attributed tolow NOX titrations and the downward mixing of ozone in the ground layer.The daily mean of Surface O3showed an increasing trend in the study area during the summer monthsand a negative correlation was observed with its precursors. The correlation of Surface O3 with temperature and wind speed for the entire summer season was found as r= +0.68, p= 4.314E-05 and r= +0.63, p.
机译:表面臭氧(表面O3)是次要污染物,在印度南部,对臭氧的研究很少。研究表明,较高的臭氧水平与较暖的日子之间有很强的相关性。在印度泰米尔纳德邦的坎亚库马里(8.0780°N,77.5410°E)对O3及其前驱物(如NO2,CO和CH4)进行了测量,在本文中,我们介绍了2010年至2014年夏季臭氧的夏季变化。在2014年夏季的所有测量日中,O3的表面都有明显的昼夜变化,但在夜间却观察到不规则的变化.0230时O3的表面形成了一个明显的次高峰,并伴有相对较强的风型。由于正常的昼夜变化不能解释这一现象,因此这种不确定的行为可能是由于NOX滴定度降低和底层臭氧的向下混合所致。夏季O3的日均值在研究区域呈上升趋势,且呈负相关观察到它的前体。整个夏季,地表O3与温度和风速的相关性为r = + 0.68,p = 4.314E-05,r = + 0.63,p。

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