雷达TREC风的三维变分同化应用与试验

万齐林; 薛纪善; 陈子通; 刘春霞

雷达TREC风的三维变分同化应用与试验

1.
中国气象局广州热带海洋气象研究所, 广东, 广州, 510080
2.
中国气象科学研究院, 北京, 100081

基金项目: "十五 "国家重点科技攻关计划项目 "中国气象数值预报技术创新研究 "(2001BA607B);科技部重点公益性研究项目 "我国登陆台风灾害的监测与预报技术研究 "(2001DIA20026)共同资助

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出版历程
- 收稿日期: 2004-09-15
- 修回日期: 2004-11-28

THE TEST OF APPLYING RADAR TREC WIND IN THREE- DIMENSIONAL VARIATIONAL ASSIMILATION

1.
Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China
2.
Chinese Academy of Meteorological Sciences, Beijing 100081, China

摘要

摘要: 介绍了雷达TREC风场在中国气象科学研究院开发的三维变分同化系统GRAPeS-3DVar中的应用,研究了GRAPeS-3DVar系统同化雷达TREC风场资料的一些基本特性,发现雷达TREC风场在GRAPeS-3DVar中有较好的应用价值,能有效地提高分析产品的质量,并通过一个热带气旋登陆变性过程的数值试验,说明了在GRAPeS-3DVar中加入雷达TREC风场也能改善预报效果。
- 雷达TREC风场 /
- 三维变分同化 /
- 数值试验
Abstract: The radar TREC wind(tracking radar echoes by correlation) was applied in three-dimensional variational assimilation system(GRAPeS-3DVar) developing by the Chinese Academy of Meteorological Sciences.Some numerical tests were performed to study the characteristics of assimilating radar TREC wind in GRAPeS-3DVar system.The result shows that the radar TREC wind was available to improve the analysis quantity in the GRAPeS-3Dvar.Also,the further test of simulating a tropical cyclone landfall process shows that the forecast was improved by assimilating the radar TREC the wind in the GRAPeS-3DVar.
- radar TREC wind /
- three-dimensional variational assimilation /
- numerical test

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参考文献(11)

[1]	SCIALOM G, LEMAITRE Y. A new analysis for the retrieval of three-dimensional mesoscale wind fields from multipleDoppler radar[J].J Atmos Oceanic Technol, 1990, 7(4): 640-665.
[2]	SUN J, FLICHER D. Recovery of three-dimensional wind and temperature fields from single-Dopple radar data[J].J Atmos Sci, 1991, 48(6): 876-890.
[3]	QIU C, XU Q. A simple adjoint method of wind analysis for single-dopple radar data[J].J Atmos Oceanic Tech, 1992, 9(5): 588-598.
[4]	SHAPIRO A, ELLIS S, SHAW J. Single-Doppler velocity retrievals with Phoenix data: Clear air and microburst wind retrievals in the planetary boundary layer[J].J Atmos Sci, 1995, 52(9): 1265-1287.
[5]	马翠平, 张培昌, 匡晓燕,等. 单多普勒天气雷达反演中尺度气旋环流场的方法[J].南京气象学院学报,2000,23(4):579-584.
[6]	邱崇践, 余金香. 多普勒雷达资料对中尺度系统短期预报的改进[J].气象学报,2000,58(2):244-249.
[7]	SMYTHE G R, ZRNIC D S. Correlation analysis of Doppler radar data and retrieval of the horizontal wind[J].J Climate and Appl Meteor, 1983, 22(2): 297-311.
[8]	TUTTLE J D, FOOTE G B. Determination of the Boundary Layer Airflow from a Single Doppler Radar[J].J Atmos Ocean Tech, 1990, 7(2): 218-232.
[9]	TUTTLE J, GALL R. A Single-Radar technique for estimating the winds in tropical cyclones[J].Bull Amer Meteor Soc, 1999, 80(4): 653-667.
[10]	张华, 薛纪善, 庄世宇, 等. GRAPeS三维变分同化系统的理想研究[J].气象学报,2004,62(1): 31-41.
[11]	王康玲, 万齐林. 南海热带气旋数值预报业务系统[A].全国热带气旋科学讨论会论文集[C].北京:气象出版社,2001.