首页> 外文期刊>Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences >Retrieval of stratospheric O_3 and NO_2 vertical profiles using zenith scattered light observations
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Retrieval of stratospheric O_3 and NO_2 vertical profiles using zenith scattered light observations

机译:利用天顶散射光观测反演平流层O_3和NO_2垂直剖面

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Daily zenith scattered light intensity observations were carried out in the morning twilight hours using home-made UV-visible spectrometer over the tropical station Pune (18°31′, 73°51′) for the years 2000-2003. These observations are obtained in the spectral range 462-498 nm for the solar zenith angles (SZAs) varying from 87° to 91.5°. An algorithm has been developed to retrieve vertical profiles of ozone (O_3) and nitrogen dioxide (NO_2) from ground-based measurements using the Chahine iteration method. This retrieval method has been checked using measured and recalculated slant column densities (SCDs) and they are found to be well matching. O_3 and NO_2 vertical profiles have been retrieved using a set of their air mass factors (AMFs) and SCDs measured over a range of 87-91.5° SZA during the morning. The vertical profiles obtained by this method are compared with Umkehr profiles and ozonesondes and they are found to be in good agreement. The bulk of the column density is found near layer 20-25 km. Daily total column densities (TCDs) of O_3 and NO_2 along with their stratospheric and tropospheric counterparts are derived using their vertical profiles for the period 2000-2003. The total column, stratospheric column and tropospheric column amounts of both trace gases are found to be maximum in summer and minimum in the winter season. Increasing trend is found in column density of NO_2 in stratospheric, tropospheric and surface layers, but no trend is observed in O_3 columns for above layers during the period 2000-2003.
机译:在2000年至2003年期间,使用自制的紫外线可见光谱仪在热带站浦那(18°31′,73°51′)上的暮光清晨进行了天顶散射光强度的每日观测。这些观测是在462-498 nm的光谱范围内获得的,其中太阳天顶角(SZAs)从87°到91.5°不等。已经开发出一种算法,可以使用Chahine迭代方法从地面测量中检索臭氧(O_3)和二氧化氮(NO_2)的垂直剖面。已使用测量和重新计算的斜柱密度(SCD)检查了此检索方法,发现它们非常匹配。 O_3和NO_2的垂直剖面已使用一组空气质量因子(AMF)和SCD进行了检索,这些空气质量因子和SCD在早晨在SZA的87-91.5°范围内测量。将通过这种方法获得的垂直剖面与Umkehr剖面和臭氧探空仪进行比较,发现它们吻合良好。在20-25 km层附近发现了大部分的柱密度。使用2000-2003年期间的O_3和NO_2以及它们的平流层和对流层对应物的每日总柱密度(TCD)进行推算。两种痕量气体的总塔,平流层塔和对流层塔的量在夏季最高,在冬季最低。在平流层,对流层和表层的NO_2柱密度发现增加的趋势,但在2000-2003年期间,在上述层的O_3柱中没有观察到趋势。

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