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Ozone Variability in the Midlatitude Upper Troposphere and Lower Stratosphere Diagnosed from a Monthly SAGE II Climatology Relative to the Tropopause

机译:根据对流层顶月刊SAGE II气候学诊断,中纬度对流层和平流层下层的臭氧变化

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摘要

[1] A midlatitude (25°–65°) monthly zonal median ozone climatology in the upper troposphere and lower stratosphere (UTLS), from 8 to 20 km with a 0.5-km vertical resolution and a 5° latitudinal resolution, is developed on the basis of version 6.2 (V6.2) ozone profile retrievals from the Stratospheric Aerosol and Gas Experiment (SAGE) II measurements from October 1984 to August 2005. To avoid mixing of the tropospheric ozone data with stratospheric values, the thermal tropopause height is used as a base altitude for developing the climatology (the monthly mean tropopause height has been added back to the climatological profile). This feature of the developed ozone climatology, together with the near global SAGE II data coverage, complements the existing ozone climatologies in the midlatitude UTLS. In addition to using this climatology to describe hemispheric differences in the UTLS ozone (the primary purpose of this paper), the database can also be used to initialize atmospheric chemistry-transport models or for satellite data retrieval. The specific new findings include (1) the differences in the vertical structure of monthly ozone evolution across the tropopause between the NH and the SH, (2) all year bimodal probability distribution functions (PDFs) of the tropopause ozone, and (3) the annual cycle of the tropopause ozone PDF with increasing (decreasing) presence of ozone-rich air leading to tropopause ozone enhancements (reductions) during spring and early summer (fall and winter). The derived climatology is shown to be consistent with the ozonesonde climatologies of Logan (1985, 1999a) in many respects, including ozone seasonal cycle at the tropopause and in the UT, the broad summer ozone maximum in the northern UT, and non-Gaussian ozone PDFs at the tropopause. This consistency strengthens the confidence in SAGE II satellite ozone remote sensing in the UTLS. The derived SAGE II midlatitude ozone climatology is compared to ozonesonde measurements at Hohenpeissenberg (47.4°N, 11°E), Germany, and Lauder (45°S, 169.7°E), New Zealand. The monthly ozone climatology data are provided as auxiliary material to this report.
机译:[1]开发了对流层和平流层下层(UTLS)中纬度(25°–65°)月度中值臭氧气候,从8至20 km,垂直分辨率为0.5 km,纬度分辨率为5°。 1984年10月至2005年8月从平流层气溶胶和气体实验(SAGE)II测量中获取的6.2版(V6.2)臭氧剖面的基础。为了避免将对流层臭氧数据与平流层值混合,使用对流层顶热高度作为发展气候学的基础高度(每月平均对流层顶高度已添加回气候资料中)。发达的臭氧气候学的这一特征,加上近乎全球的SAGE II数据覆盖,补充了中纬度UTLS中现有的臭氧气候。除了使用这种气候来描述UTLS臭氧中的半球差异(本文的主要目的)之外,该数据库还可以用于初始化大气化学传输模型或用于卫星数据检索。具体的新发现包括(1)NH和SH之间对流层顶每月臭氧演化的垂直结构差异;(2)对流层顶臭氧的全年双峰概率分布函数(PDFs);以及(3)对流层顶臭氧PDF的年度周期随着富含臭氧的空气的存在(减少)而导致,在春季和初夏(秋季和冬季)导致对流层顶臭氧的增强(减少)。在许多方面,得出的气候学与洛根的臭氧探空仪气候一致(1985年,1999a),包括对流层顶和密西根州的臭氧季节性周期,北密歇根州北部的夏季宽泛臭氧最大值和非高斯臭氧层PDF在对流层顶。这种一致性增强了人们对UTLS中SAGE II卫星臭氧遥感的信心。在德国的Hohenpeissenberg(北纬47.4°,东经11°)和新西兰的Lauder(北纬45°,东经169.7°),将得到的SAGE II中纬度臭氧气候与臭氧探空仪的测量结果进行了比较。每月的臭氧气候数据作为本报告的辅助材料。

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