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中国不同地区剩余臭氧及臭氧探空订正因子

郑向东 田宏民 刘梦琪

郑向东, 田宏民, 刘梦琪. 中国不同地区剩余臭氧及臭氧探空订正因子[J]. 空间科学学报, 2017, 37(5): 564-573. doi: 10.11728/cjss2017.05.564
引用本文: 郑向东, 田宏民, 刘梦琪. 中国不同地区剩余臭氧及臭氧探空订正因子[J]. 空间科学学报, 2017, 37(5): 564-573. doi: 10.11728/cjss2017.05.564
ZHENG Xiangdong, TIAN Hongmin, LIU Mengqi. Residual Ozone and Ozonesonde Correction Factor over Different Sites of Chinaormalsize[J]. Journal of Space Science, 2017, 37(5): 564-573. doi: 10.11728/cjss2017.05.564
Citation: ZHENG Xiangdong, TIAN Hongmin, LIU Mengqi. Residual Ozone and Ozonesonde Correction Factor over Different Sites of Chinaormalsize[J]. Journal of Space Science, 2017, 37(5): 564-573. doi: 10.11728/cjss2017.05.564

中国不同地区剩余臭氧及臭氧探空订正因子

doi: 10.11728/cjss2017.05.564
基金项目: 

公益性气象行业专项项目资助(GYHY201106041)

详细信息
    作者简介:

    郑向东,E-mail:zhengxd@camscma.cn

  • 中图分类号: P352

Residual Ozone and Ozonesonde Correction Factor over Different Sites of Chinaormalsize

  • 摘要: 根据中国不同地点臭氧探空数据,研究气球炸点臭氧浓度定值(CMR)法、卫星(SBUV和MLS)纬向平均法确定的剩余臭氧Ωres及其对订正因子Cref的影响,同时检验臭氧垂直分布对Cref的贡献.结果显示: CMR法对气球炸点高度依赖性明显,且易高估Ωres使Cref整体低于100%;卫星纬向平均Ωres对气球炸点高度不敏感,但在中国东部的臭氧总量高值区或青藏高原及低纬度臭氧低值地区,Ωres呈现近10DU以上低值,这是经向臭氧总量及其垂直分布差异在卫星遥感数据上的反映.地面到100hPa的对流层臭氧(Ωtro),100~10hPa的平流层臭氧(Ωstr)以及10hPa以上的ΩresCref贡献平均分别为(16±3.4)%,(65±2.3)%,(19±3.3)%.表明基于Cref评估或订正探空仪平流层臭氧测值时,需考虑对流层臭氧及确定Ωres方法的影响.卫星纬向平均法,特别是近似实测的SBUV臭氧廓线的值适用于确定Ωres.

     

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出版历程
  • 收稿日期:  2016-09-21
  • 修回日期:  2017-05-24
  • 刊出日期:  2017-09-15

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