高原气象

高原气象 >

2017 , Vol. 36 >Issue 5: 1201 - 1208

DOI: https://doi.org/10.7522/j.issn.1000-0534.2016.00106

论文

青藏高原臭氧谷的分布及其与太阳辐射的关系

  • 焦铂洋 ,
  • 苏昱丞 ,
  • 郭胜利 ,
  • 郭栋 ,
  • 施春华 ,
  • 李婧媛 ,
  • 苍中亚 ,
  • 傅帅
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  • 空间天气研究所/南京信息工程大学数学与统计学院, 南京 210044;福建省气象培训中心, 福州 350007;南京信息工程大学气象灾害教育部重点实验室/气候与环境变化国际合作联合实验室/气象灾害预报预警与评估协同创新中心, 南京 210044;中国科学院国家天文台, 北京 100012

收稿日期: 2016-06-23

  网络出版日期: 2017-10-28

基金资助

国家自然科学基金项目（61573193, 91537213, 41305039, 41675039）；江苏高校优势学科建设工程项目（PAPD）

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Distribution of Ozone Valley and Its Relationship with Solar Radiation over the Qinghai-Tibetan Plateau

  • JIAO Boyang ,
  • SU Yucheng ,
  • GUO Shengli ,
  • GUO Dong ,
  • SHI Chunhua ,
  • LI Jingyuan ,
  • CANG Zhongya ,
  • FU Shuai
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  • Institute of Space Weather/School of Mathematics and Statistics, Nanjing University of Information Science and Technology, Nanjing 210044, China;Training Center of Fujian Meteorology, Fuzhou 350007, China;Nanjing University of Information Science and Technology Key Laboratory of Meteorological Disaster, Ministry of Education(KLME)/Joint International Research Laboratory of Climate and Environment Change(ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters(CIC-FEMD), Nanjing 210044, China;National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012, China

Received date: 2016-06-23

  Online published: 2017-10-28

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摘要

使用2005-2015年夏季Aura卫星微波临边探测器（MLS）逐日臭氧观测资料, 讨论了夏季青藏高原臭氧低值区的三维分布。研究发现, 青藏高原臭氧不仅在对流层顶附近存在着臭氧低值区, 而且在平流层上层（20~1 hPa）也存在显著的低值区。高原区上空50%以上的臭氧存在于21.5~1.2 hPa的范围内, 因此平流层上层高原臭氧低值对高原臭氧谷来说也很重要。使用合成分析法对MLS夏季北半球昼夜臭氧进行研究, 结果表明该低值区仅存在于白天。根据高原区平流层上层臭氧模拟数据的集合经验模态分解, 得到IMF4的平均频率为0.09, 平均周期为11.1年, 正好对应太阳活动最强的周期。说明太阳辐射是影响高原平流层上层臭氧低值中心的一个因素。

关键词： 青藏高原; 平流层中上层; 臭氧低值中心; 太阳辐射

本文引用格式

焦铂洋 , 苏昱丞 , 郭胜利 , 郭栋 , 施春华 , 李婧媛 , 苍中亚 , 傅帅 . 青藏高原臭氧谷的分布及其与太阳辐射的关系[J]. 高原气象, 2017 , 36(5) : 1201 -1208 . DOI: 10.7522/j.issn.1000-0534.2016.00106

Abstract

Using Aura satellite 10 years (2005-2015) summer (from June to August) microwave limb sounder (MLS) daily ozone observation data, the three-dimensional distribution of the core of ozone valley over the Qinghai-Tibetan Plateau in summer is analyzed.The results show that the ozone valley in the Qinghai-Tibetan Plateau is not only in the tropopause, but also in the upper stratosphere (20~1 hPa).More than 50% of the ozone over the plateau is in the range of 21.5~1.2 hPa, so for ozone valley upper stratospheric ozone plateau low plateau is also very important.Then by using synthetic analysis method, MLS ozone in the Northern Hemisphere summer day and night were compared, and we can see there is a core of ozone valley on the plateau during the day.Next, by using Ensemble Empirical Mode Decomposition (EEMD) to process total ozone analog data in the Plateau, the average frequency of IMF4 is 0.09, that is to say the average period is 11.1 years, exactly correspond to the strongest solar activity cycle.So solar activity is a factor for the core of ozone valley in the plateau upper stratosphere.

Key words： Qinghai-Tibetan plat; The middle and upper; The core of ozone va; Solar radiation

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