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首页> 外文期刊>International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences >SPATIAL AND TEMPORAL VARIATION OF TOTAL AND TROPOSPHERIC OZONE COLUMNS OVER CHINA
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SPATIAL AND TEMPORAL VARIATION OF TOTAL AND TROPOSPHERIC OZONE COLUMNS OVER CHINA

机译:中国总体和对流层臭氧柱的空间和时间变化

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In this study, total ozone columns collected from nine sites of the AErosol RObotic NETwork (AERONET) in China are used to evaluate total ozone column monthly mean products of the Ozone Monitoring Instrument (OMI). The results show the correlated coefficient of the two datasets is 0.95. The long temporal variations and spatial distributions of the monthly mean products of the total ozone columns and tropospheric ozone columns in spring, summer, autumn and winter were plotted. The result shown in the pictures indicate that the total ozone columns gradually increase from low latitude to high latitude, reach the maximum value in winter and spring in Northeast China, and the values in Qinghai-Tibet Plateau are lower than those of other regions of the same latitude. The monthly mean of total ozone columns at low latitude have no obvious seasonal variation. With the increase of latitude, the seasonal variation of monthly mean products of total ozone column becomes more and more obvious. Tropospheric ozone columns are the highest in summer, followed by spring and autumn, and the lowest in winter, which are mainly concentrated in the more developed areas in eastern China. The lowest value of tropospheric ozone column in China occurs in the Qinghai-Tibet Plateau in winter and the highest value in North China in summer. The study indicates that the total ozone columns vary with latitude while tropospheric ozone columns are more susceptible to human activities and natural conditions.
机译:在本研究中,从中国九个地点收集的总臭氧柱用于评估臭氧监测仪(OMI)的臭氧柱月平均值。结果显示了两个数据集的相关系数为0.95。绘制了春季,夏季,秋季和冬季总臭氧柱和对流层臭氧柱的月平均值的长时间变化和空间分布。图片中所示的结果表明,总臭氧柱从低纬度逐渐增加到高纬度,达到了中国东北冬季和春季的最大值,青藏高原的价值低于其他地区的价值相同的纬度。低纬度总臭氧柱的月平均值没有明显的季节性变化。随着纬度的增加,每月臭氧柱的月平均产物的季节变化变得越来越明显。对流层臭氧柱是夏季最高的,其次是春季和秋季,冬季最低,主要集中在中国东部的越来越多的地区。中国对流层臭氧柱的最低价值在冬季青藏高原和夏季华北地区的最高价值。该研究表明,总臭氧柱随纬度而变化,而对流层臭氧柱更容易受到人类活动和自然条件的影响。

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