Wang Hongyan, Liu Liping, Wang Gaili, et al. Development and application of the Doppler weather radar 3-D digital mosaic system. J Appl Meteor Sci, 2009, 20(2): 214-224.
Citation: Wang Hongyan, Liu Liping, Wang Gaili, et al. Development and application of the Doppler weather radar 3-D digital mosaic system. J Appl Meteor Sci, 2009, 20(2): 214-224.

Development and Application of the Doppler Weather Radar 3-D Digital Mosaic System

  • Received Date: 2008-03-04
  • Accepted Date: 2009-02-11
  • Publish Date: 2009-04-30
  • Today, most radar sites of the CINRAD have been established, and there is good condition to transmit radar base data to the regional center. To fully utilize the advantage of the Doppler weather radar network, and improve the capability of mesoscale disaster weather early warning, study about weather radar 3-D mosaic has been made in recent years, and the Doppler weather radar 3-D digital mosaic system is developed for the first time in China based on these research results. It introduces the design, system structure, main function modules, data process flow, and corresponding algorithms of the system, analysis software performance, practicality and reliability of the mosaic results, study methods to discriminate two important factors affect the mosaic results.The system includes the following modules: Base data loading, data time matching, data quality controlling, coordinates conversion of single site base data to Cartesian coordinates, reflectivity mosaic for all sites in the region, and the generation of series of derived products. It can provide quality controlled base data, 3-D reflectivity grid data of single site, 3-D mosaic reflectivity and some derived products base on mosaic base data, which are useful not only for operational work, but also for scientific research. It can run real time for the region with around fifteen radars, at intervals about 6 minutes, with the horizontal resolution of about 1 km, and at least 20 vertical height levels.Operational running on trial proves that the system is steady. Case study results show that the 3-D mosaic result with high time and spatial resolution is reliable, it provides advantage for analyzing mesoscale and small-scale severe weather, and supplies data basis for developing now-casting and some other works. Besides, the observation errors and position errors are two important cases which influence the mosaic results, and they can be determined easily by analyzing outputs of the system itself. The system is running on trial currently. It's planned to upgrade the system for business, after adding some functions and useful derived products in the near future.
  • Fig. 1  Contrast of reflectivity and velocity without quality control (a) and with quality control (b) at elevation of 0.5°

    Fig. 2  Contrast of compositer eflectivity and vertical cross section from volume scan and 3-D mosaic radar data(R=240 km) (a) composite reflectivity from RPG (black line is the position of cross section) , (b) composite reflectivity from 3-D digital mosaic system, (c) cross section from RPG, (d) cross section from 3-D mosaic data

    Fig. 3  Contrast of reflectivity at the height of 5 km between single radar and mosaic

    (a) mosaic reflectivity, (b) reflectivity of Meizhou radar, (c) reflectivity of Shenzhen radar, (d) reflectivity of Shaoguan radar, (e)reflectivity of Shantou radar

    Fig. 4  Results of 3-D digital mosaic system and national radar mosaic system

    (a) composite reflectivity generated by the 3-D digital mosaic system, (b) composite reflectivity from national radar mosaic system

    Fig. 5  Relativity between the echo of Beijing , Tianjin and Qinhuangdao radar

    (a) reflectivity at 1.5 °elevation produced by SA radar software of Beijing, Tianjin and Qinhuangdao, (b) mosaic reflectivity at 3 km height, (c) reflectivity of Beijing at 3 km height, (d) reflectivity of Tianjin at 3 km height, (e) reflectivity of Qinhuangdao at 3 km height

    Table  1  Correlation of radar echo between Beijing and Tianjin

    Table  2  Correlation of radar echo between Beijing and Qinhuangdao

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    • Received : 2008-03-04
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    • 录用日期:  2009-02-11
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    • Published : 2009-04-30

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