Analysis of atmospheric boundary ozone profiles in winter in hinterland of Taklimakan Desert

被引:0
|
作者
He, Qing [1 ,2 ]
Yang, XingHua [1 ,2 ]
Mamtimin, Ali [1 ,2 ]
Huo, Wen [1 ,2 ]
Liu, Qiang [1 ,2 ]
机构
[1] China Meteorol Adm, Inst Desert Meteorol, Xinjiang 830002, Peoples R China
[2] Taklimakan Desert Atmosphere & Environm Observat, Xinjiang 841000, Peoples R China
来源
SCIENCES IN COLD AND ARID REGIONS | 2011年 / 3卷 / 04期
关键词
atmospheric boundary layer; ozone profiles; Taklimakan Desert;
D O I
10.3724/SP.J.1226.2011.00358
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
In order to reveal the variation characteristics of ozone (O-3) concentration in the atmosphere boundary layer over a desert in winter, an observation experiment was carried out in the Tazhong area by means of a tethered balloon during January 18-25, 2008. The vertical distribution of O-3 concentration and its correlation with temperature and humidity were analyzed based on experimental observation data and related data. Results show that: (1) The concentration of O-3 mainly ranges from 10 to 50 mu g/L, with a maximum of 56.1 mu g/L, minimum of 2.6 mu g/L, and a daily average concentration of 34.4 mu g/L. (2) O-3 profiles can be divided into three types: peak, uniform, and growth, where uniform accounts for the majority. (3) Temperature and moisture are influential on O-3 concentrations in atmospheric boundary layer. Temperature inversion and water vapor increase in an atmospheric boundary layer leads to a decrease of O-3. (4) O-3 concentration has an obvious daily change in Tazhong. It is lower at night, begins to increase after sunrise, and reaches a maximum at noon. The maximum appears at 17:00 BJT (Beijing Time), and the minimum appears at 08:00 BJT.
引用
收藏
页码:358 / 365
页数:8
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