[1]钟美,皮波,佘勇,等.FY-3B TOU与Aura OMI卫星臭氧总量产品的比对分析[J].气象研究与应用,2021,42(02):29-34.[doi:10.19849/j.cnki.CN45-1356/P.2021.2.06]
　Zhong Mei,Pi Bo,She Yong,et al.Comparative analysis of total ozone products between FY-3B TOU and Aura OMI satellite[J].Journal of Meteorological Research and Application,2021,42(02):29-34.[doi:10.19849/j.cnki.CN45-1356/P.2021.2.06]
点击复制

FY-3B TOU与Aura OMI卫星臭氧总量产品的比对分析()
分享到：

气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第42卷
期数:
2021年02期
页码:
29-34
栏目:
研究论文
出版日期:
2021-07-06

文章信息/Info

Title:
Comparative analysis of total ozone products between FY-3B TOU and Aura OMI satellite
作者:
钟美1;  皮波2;  佘勇3;  郑向东4
1. 重庆市气象信息与技术保障中心, 重庆 401147;
2. 民航重庆空管分局, 重庆 401120;
3. 成都信息工程大学, 成都 610225;
4. 中国气象科学研究院, 北京 100081
Author(s):
Zhong Mei1;  Pi Bo2;  She Yong3;  Zheng Xiangdong4
1. Chongqing Meteorological Information and Technology Support Center, Chongqing 401147;
2. Civil Aviation Chongqing Air Traffic Control Branch, Chongqing 401120;
3. Chengdu University of Information Technology, Chengdu 610225;
4. Chinese Academy of Meteorological Sciences (CAMS) China Meteorological Administration, Beijing, 100081
关键词:
FY-3B TOU; Aura-OMI; OMTO3e; 臭氧总量; 相对偏差RD; 时空分布
Keywords:
FY-3B TOU; Aura-OMI OMTO3e; total ozone; relative difference(RD); space-time distribution
分类号:
P412.27
DOI:
10.19849/j.cnki.CN45-1356/P.2021.2.06
摘要:
通过FY-3B TOU与Aura OMI卫星臭氧总量产品的比对分析，检验FY-3B TOU臭氧总量产品的适用性。结果显示，两者的相对偏差（RD）在赤道、南北半球中纬度大部分地区为2%~4%，而在南北极区扩到4%~6%和8%~10%，从赤道到两极RD随纬度升高而增大；除南北极区外，其余地区RD月平均值均呈现出明显的季节变化特征，尤其南半球中纬度地区的季节特征更为显著；赤道地区RD值随卫星臭氧总量的变化波动较小，基本稳定在0.1%~2.9%，其余地区仅卫星臭氧总量在230~500DU之间时，RD才出现相对稳定的波动，可见除赤道地区外RD在不同区域对卫星臭氧总量值有一定程度的依赖性；南北极区太阳天顶角（SZA）在45°~65°期间，RD随SZA增大均呈正的下降趋势，在70°~80°之间均呈现小幅度的回升，总体来看，TOU臭氧总量RD值受SZA变化情况并不明显。
Abstract:
The total ozone products of FY-3B TOU (November 2010 to December 2016) were verified and analyzed by OMTO3e, the total ozone product of Aura-OMI satellite. The results show that RD values of the equator and in most of the middle latitudes of northern and southern hemispheres are in the range of 2%~4%, and the RD values in the north and south polar regions are in the range of 4%~6% and 8%~10%. In different spaces from the equator to the poles, RD increases with the increase of latitude. Except for the north and south polar regions, the monthly mean RD shows obvious seasonal variation characteristics, especially in the middle latitude region of the southern hemisphere. The RD value in the equatorial region fluctuates slightly with the variation of the total satellite ozone, which is basically stable in the range of 0.1%~2.9%. In the other regions, RD fluctuates is relatively stable only when the total satellite ozone is between 230~500 DU. The RD shows a certain degree of dependence on the total satellite ozone value in different regions. The RD shows a positive downward trend with the increase of the solar zenith angle (SZA) in the period of 45°~65° in the south and north polar regions, and a slight upward trend between 70°~80°. To sum up, the RD of total ozone between TOU and OMTO3e is not significantly affected by SZA.

参考文献/References:

[1] WMO. Scientific Assessment of Ozone Depletion:2006, Global Ozone Research and Monitoring Project-Report No.50[R]. Geneva, Switzerland,2007.
[2] WMO, UNEP. Assessment for decision maker:scientific assessment of ozone depletion:2014//Global Ozone Research and Monitoring Project-Report No.56[R]. Geneva, Switzerland, 2014.
[3] Shine K P. Atmospheric ozone and climate change[J]. Ozone:Science Engineering. 2001,23(6):429-435.
[4] 杜君平,朱玉霞,刘锐,等.基于OMI数据的中国臭氧总量时空分布特征[J].中国环境监测,2014,30(2):191-196.
[5] 肖钟湧,江洪.亚洲地区OMI和SCIAMACHY臭氧柱总量观测结果比较[J].中国环境科学,2011,31(4):529-539.
[6] 李天奕.基于OMI和TOMS的大气臭氧柱总量时空变化的研究[D].中国科学技术大学,2011,4-6.
[7] 莫伟华,陈燕丽,莫建飞,等.卫星遥感在广西气象服务中应用的回顾与展望[J].气象研究与应用,2020,41(4):81-87.
[8] 黄永璘,农民强,孙涵.基于FY-3A/MERSI的洪涝灾害遥感监测初探[J].气象研究与应用,2009,30(2):59-61,112.
[9] 陈兴鹃,黄淑娥,樊建勇,等.基于FY-3A/VIRR卫星资料的江西省大雾遥感监测[J].气象研究与应用,2018,39(1):91-95,153.
[10] 杨双艳,周顺武.对流层顶研究回顾[J].气象科技,2010,38(2):145-151.
[11] 黄荣,刘日胜,刘国忠等.FY3极轨卫星资料在暴雨短时预报中的应用分析[J].气象研究与应用,2018,39(2):41-44,71,144.
[12] 杨忠东,卢乃锰,施进明,等.风云三号卫星有效载荷与地面应用系统概述[J].气象科技进展,2013,3(4):6-12.
[13] 刘年庆,黄富祥,王维和.2011年春季北极地区臭氧低值事件的卫星遥感监测[J].科学通报,2011,56(27):2315-2318.
[14] Bai K X,Liu C H,Shi R H,et al. Global validation of FY-3A total ozone unit(TOU)total ozone columns using ground-based Brewer and Dobson measurements[J]. International Journal of Remote Sensing, 2013,34(14):5228-5242.
[15] Wang W H, Flynn L, Zhang X Y, et al. Cross-Calibration of the Total Ozone Unit(TOU) with the Ozone Monitoring Instrument(OMI) and SBUV/2 for environmental applications[J]. Advonce in Meteorological Science and Technology,2013,3(4):97-107.
[16] 江芳,王维和,王咏梅,等.FY-3气象卫星紫外臭氧总量探测仪辐亮度在轨定标与反演结果分析[J].地球物理学报,2012,55(3):760-767.
[17] 王咏梅,王英鉴,王维和,等.FY-3卫星紫外臭氧总量探测仪[J].科学通报,2009,54(23):3778-3783.
[18] Bhartia P K. OMI Algorithm Theoretical Basis Document, Volume II[R]. NASA Goddard Space Flight Center Greenbelt, Maryland, USAATBD-OMI-02, 2002.
[19] Antón M, Kroon M, López M,et al. Total ozone column derived from GOME and SCIAMACHY using KNMI retrieval algorithms:Validation against Brewer measurements at the Iberian Peninsula[J]. JOURNAL OF GEOPHYSICAL RESEARCH, 2011,116(D22303).
[20] Li L,Zhang X D,Chen S,et al. Validation study of FY-3A-TOU total ozone using ground-based data[J]. Chinese Journal of Spase Science,2015,35(6):696-706.
[21] 王维和,张兴赢,安兴琴,等.风云三号气象卫星全球臭氧总量反演和真实性检验结果分析[J].科学通报,2010,55(17):1726-1733.
[22] 郑向东,韦小丽.中国4个地点地基与卫星臭氧总量长期观测比较[J].应用气象学报,2010,21(1):1-10.

备注/Memo

备注/Memo:
收稿日期:2021-05-09。
基金项目:“基于气象+大数据平台环境的重庆及周边省份雷达数据共享方法实现”（QNJJ-202105）
作者简介:钟美(1989-),女,四川人,硕士,助理工程师,主要从事气象信息技术工作。E-mail:1055208211@qq.com
更新日期/Last Update: 1900-01-01