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SONG Xiaojiang, YANG Xuelian, XING Jianyong. The test of typhoon forescast improve by 3d variational assimilation of GPS occulation material[J]. Haiyang Xuebao, 2013, 35(5): 67-75. doi: 10.3969/j.issn.0253-4193.2013.05.007
Citation: SONG Xiaojiang, YANG Xuelian, XING Jianyong. The test of typhoon forescast improve by 3d variational assimilation of GPS occulation material[J]. Haiyang Xuebao, 2013, 35(5): 67-75. doi: 10.3969/j.issn.0253-4193.2013.05.007

The test of typhoon forescast improve by 3d variational assimilation of GPS occulation material

doi: 10.3969/j.issn.0253-4193.2013.05.007
  • Received Date: 2012-07-06
  • In recent years, along with the rapid development of atmospheric sounding technology, the application of a series of high spatial and temporal resolution unconventional data,such as GPS occulation refractive index,has compensated the shortages of Marine observation data. This paper presents the utility of GPSRO COSMIC material in meso-scale model. Cloud and precipation suffer less inpact on COSMIC,in addition COSMIC has high precision and high vertically resolution,so it could improve the initial field in model and then raise the prediction accuracy. With incorporated the meso-scale meterological model, V3.0.1 WRF,and 3d variational assimilation system(3DVAR), the MORAKOT landing process is simulated by using NCEP,GTS and COSMIC. Experiment results show: assimilation COSMIC could improve the rainstorm forecast in certain degree,and meanwhile through to the preliminarily discussion for each diagnosis quantity and different levels of wind field,it considers the assimilation data could play a certain indicate role for typhoon intensity,pathway and precipation by making better forecast results for the amount.
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  • Kuo Y-H. Comparison of GPS radio occultation soundings with radiosondes comparison of GPS radio occultation soundings with radiosondes[J]. Geophysical Research Letters,2005,32, L05817: 4.
    Huang C-Y, Kuo Y H, Chen S-H.Improvements on typhoon forecast with assimilated GPS occultation refractivity[J].Weather and Forecasting,2005,6:931-953.
    Sokolovskiy S V,Rocken C,Hunt D.GPS profiling of the lower troposphere from space:inversion and demodulation of the open-loop radio occultation signals[J].Geophysical Research Letters, 2006(14):1029.
    丁金才.GPS气象学及其应用[M].北京:气象出版社,2009:11.
    Le Dimet F,Talagrand O.Variational algorithms for analysis and assimilation of meteorologicaI observations:TheoreicaI aspects[J].Tellus,1986,38(A):97-110.
    Kuo Y-H. Inversion and error estimation of GPS radio occultation data[J]. Journal of the Meteorological Society of Japan, 2004,82 (1):507-531.
    Jagadheesha D, Simon B, Pal P-K. A new technique for estimation of lower-tropospheric temperature and water vapor profiles from radio occultation refractivity[J]. Journal of Atmospheric and Oceanic Technology,2009,6:1075-1089.
    苟小平,符养,郭粤宁,等.COSMIC计划及掩星数据误差分析[J].气象科学,2009,3:348-354.
    唐细坝,薛纪善.COSMIC资料在GRAPES全球三维变分同化系统的初步研究[J].热带气象学报,2009,25(5): 521-531.
    庄世宇,薛纪善,朱国富.GRAPES全球三维变分同化系统——基本设计方案与理想试验[J].大气科学,2005,29(26): 872-884.
    丁一汇.高等天气学[M].北京:气象出版社,2005:20-300.
    彭治班,刘建文,郭虎,等.国外强对流天气的应用研究[M].北京:气象出版社,2001:89-95.
    励申申,寿绍文.台风区和外围暴雨区的旋转风散度风动能收支[J].南京气象学院学报,1997,20(1):108-113.
    林秀雯. 莫拉克台风降雨分析[R]//2009年海峡两岸气象科学技术研讨会论文集.北京:中国气象学会,2009:1-50.
    徐丽丽,郑晓琴,邓小东,等.0908号台风"莫拉克"路径异常及造成台南暴雨灾害的诊断分析[J].海洋预报,2010,27:45-52.
    李波,费建芳,黄小刚. 0908号台风"莫拉克"异常路径的诊断分析与数值模拟[R]//第27届中国气象学会年会灾害天气研究与预报分会场论文集. 北京:中国气象学会,2010:1-100.
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