Effects of elevated humidity on stratospheric ozone content in the tropics

Chukwuebuka Stephen Ejimofor, E. Okoro, W. T. Sivla
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引用次数: 1

Abstract

This study examines the effects of elevated humidity on stratospheric ozone content in the tropics, a case study of Nigeria. The specific stations in Nigeria studied with their co-ordinate include Makurdi (7.7°N 8.5°E), Maiduguri (11.9°N 13.2°E), Kano (12.0°N 8.5°E), Port-Harcourt (4.9°N 7.0°E) and Lagos (6.5°N 3.4°E). Using monthly mean stratospheric ozone data from Earth Probe Total Ozone Mass Spectroscopy (EPTOMS) together with humidity and temperature data from the Nigerian Meteorological Agency (NIMET), studies were carried out over the five stations for a period of fifteen years (1998-2012). The results show that elevated humidity cools the stratosphere, slowing down the rate of chemical reactions that destroy ozone, thereby resulting to more ozone amount. Ozone variation is latitude dependent with more variations in station observed in the north. Using Spearman’s Rank Correlation Coefficient analysis, it was equally observed that ozone and temperature are strongly anti-correlated in Port Harcourt, Makurdi and Lagos stations (r = -0.8531, -0.7832, and -0.8759, respectively); and positively correlated in Maiduguri and Kano stations (r = 0.3776 and 0.4965, respectively). The positive correlation may be attributed to the high dehydration of water vapor in those stations. Results also revealed that ozone and humidity are positively correlated (r = 0.9073, 0.9021, 0.7133, 0.7552, and 0.7692), for Port Harcourt, Makurdi, Maiduguri, Lagos, and Kano. Both ozone and humidity attain maximum during wet season and minimum during the dry season in Nigeria. The implication of more humidity in the wet season is due to the evaporation of raindrops and surface puddles. The implication of more ozone concentration in the wet season may be attributed to the transportation of ozone from the influence of Brewer-Dobson Circulation (BDC). Again it was found out that temperature and humidity are negatively correlated. Consequently, our findings show that, at elevated humidity, the surface temperature is low with more stratospheric ozone content. Key words: Humidity, stratospheric ozone, temperature, rainfall.
热带地区湿度升高对平流层臭氧含量的影响
本研究以尼日利亚为例,探讨了热带地区湿度升高对平流层臭氧含量的影响。尼日利亚的具体观测站包括马库尔迪(7.7°N 8.5°E)、迈杜古里(11.9°N 13.2°E)、卡诺(12.0°N 8.5°E)、哈科特港(4.9°N 7.0°E)和拉各斯(6.5°N 3.4°E)。利用地球探测总臭氧质谱仪(EPTOMS)的月平均平流层臭氧数据以及尼日利亚气象局(NIMET)的湿度和温度数据,在五个站点进行了为期15年(1998-2012)的研究。结果表明,湿度升高使平流层降温,减缓破坏臭氧的化学反应的速度,从而导致更多的臭氧量。臭氧变化与纬度有关,在北方观测到的台站变化较多。Spearman秩相关系数分析显示,哈考特港、马库尔迪和拉各斯站臭氧与温度呈强反相关(r分别为-0.8531、-0.7832和-0.8759);与迈杜古里站和卡诺站正相关(r分别为0.3776和0.4965)。正相关可能是由于这些站点的水汽脱水程度高。哈科特港、马库尔迪、迈杜古里、拉各斯和卡诺的臭氧与湿度呈显著正相关(r = 0.9073、0.9021、0.7133、0.7552和0.7692)。尼日利亚的臭氧和湿度在雨季达到最大值,在旱季达到最小值。雨季湿度增加的含义是由于雨滴和地表水坑的蒸发。雨季臭氧浓度升高可能是由于布鲁尔-多布森环流(BDC)对臭氧的输送。再次发现温度与湿度呈负相关。因此,我们的研究结果表明,在湿度升高时,地表温度较低,平流层臭氧含量较高。关键词:湿度,平流层臭氧,温度,降雨。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
International Journal of Physical Sciences
International Journal of Physical Sciences 综合性期刊-综合性期刊
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4
审稿时长
24 months
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