首页> 外文期刊>Journal of Earth System Science >Yearly variation and annual cycle of total column ozone over New Delhi (29°N, 77°E), India and Halley Bay (76°S, 27°W), British Antarctic Survey Station and its effect on night airglow intensity of OH(8, 3) for the period 1979–2005
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Yearly variation and annual cycle of total column ozone over New Delhi (29°N, 77°E), India and Halley Bay (76°S, 27°W), British Antarctic Survey Station and its effect on night airglow intensity of OH(8, 3) for the period 1979–2005

机译:英国南极测量站,新德里(29°N,77°E),印度和哈雷湾(76°S,27°W),英国南极测量站的总柱臭氧的年变化和年循环及其对OH夜间气辉强度的影响8,3)为1979-2005年

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摘要

A critical analysis made on the long-term monthly, seasonal, yearly variation and annual cycle of total column ozone (TCO) concentration at New Delhi (29°N, 77°E), India and Halley Bay (76°S, 27°W), a British Antarctic Service Station reveals more decline in yearly mean ozone concentration at Halley Bay than at New Delhi from 1979 to 2005. The nature of variations of monthly mean TCO during the months of August and September was the most identical with that of yearly mean ozone values at New Delhi and Halley Bay, respectively, for the same period. Annual cycles of TCO over these stations are completely different for the above period. The effect of O3 depletion on night airglow emission of OH(8, 3) line at New Delhi and Halley Bay has been studied. Calculations based on chemical kinetics show that the airglow intensity of OH(8, 3) has also been affected due to the depletion of O3 concentration. The yearly variations and annual cycle of intensities of OH(8, 3) line for the above two stations are depicted and compared. It has been shown that the rate of decrease of intensity of OH(8, 3) line was comparatively more at Halley Bay due to dramatic decrease of Antarctic O3 concentration.
机译:对新德里(29°N,77°E),印度和哈雷湾(76°S,27°)的总柱臭氧(TCO)浓度的长期每月,季节性,年度变化和年度周期进行了严格的分析W),英国南极服务站显示,1979年至2005年,哈雷湾的平均臭氧浓度下降幅度大于新德里。八月和九月的月平均TCO变化性质与图5的最一致。同期,新德里和哈雷湾的年平均臭氧值。在上述期间,这些站点的TCO年度周期完全不同。研究了O3 耗竭对新德里和哈雷湾的OH(8,3)线夜间气辉发射的影响。基于化学动力学的计算表明,OH(8,3)的气辉强度也受到O3 浓度降低的影响。描绘并比较了以上两个站的OH(8,3)线强度的年变化和年周期。结果表明,由于南极O3浓度的急剧降低,哈雷湾的OH(8,3)线强度下降的速率相对较大。

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