Wang Lirong, Bian Tao, Su Yuntao, et al. The application of clear air echo to early warning of severe convective weather. J Appl Meteor Sci, 2010, 21(5): 606-613.
Citation: Wang Lirong, Bian Tao, Su Yuntao, et al. The application of clear air echo to early warning of severe convective weather. J Appl Meteor Sci, 2010, 21(5): 606-613.

The Application of Clear air Echo to Early Warning of Severe Convective Weather

  • Received Date: 2009-11-16
  • Rev Recd Date: 2010-07-08
  • Publish Date: 2010-10-31
  • Using Doppler weather radar data, two methods are implemented to estimate the divergence of environmental wind field. The first method is radial velocity image qualitative identification, through which the wind divergence is qualitatively judged by calculating the difference between positive and negative radial velocity area, and the wind speed given by comparing the value of positive and negative radial velocity in the same range rings. The other is EVAD (Extended Velocity Azimuth Display) quantitative analysis, which estimates the divergence of each level in 10—50 km around radar. They are applied in the analysis of two strong convective weather processes occurred in August 2009. The relationships between clear air echo characteristics, divergence in different levels and the time of convection appearance are statistically investigated by analyzing 50 processes from May to September during 2005 to 2008. It's found that clear air echo appears within 50 km from radar center, the reflectivity are 10—20 dBZ, and the radial velocity is about±5 m/s. There are always convergences in low levels before convective weather, so it can be used as indicator of convergent environment field when consecutive five convergences appear on low level. As the altitude lowers, convergence happens ahead of convective weather much more, and on the level of 0.5 km, the forecast time of simple rainstorm can bring forward longer than that of simultaneous multiform convective weather.
    Based on the results, a severe convective weather automatic warning system (SWEAWAR) is established and run on trial from June to August of 2009 except for 5 days without radar records. Among the 57 warnings, the hit ratio is 88.9% and false warnings ratio is 29.8%, the critical success index for the early warning is 64.5% and the convergence occurs 7.1 hours ahead of the convective weather on average. The SWEAWAR system seldom misses but generate quite a few false warnings too. Overall, it can help to reduce the missing report rate and improve forecast of severe convective weather.
  • Fig. 1  The radial velocity PPIs from 22:30 3 August to 08:30 4 August 2009 (elevaton is 0.5°, the interval of adjacent rings is 25 km)

    Fig. 2  The time series of the divergence at different height from 19:54 3 August to 02:36 4 August in 2009

    Fig. 3  The time series of the divergence at different height from 07:54 to 13:00 on 4 August 2009

    Fig. 4  The time series of the radial velocity PPIs from 12:00 to 15:30 on 27 August 2009 (the elevation is1.5°, the interval of adjacent rings is 25 km)

    Fig. 5  The time series of the divergence at different height from 11:54 to 19:00 on 27 August 2009

    Table  1  The rings in the height of 0—500 m in each elevation angles

    Table  2  The analysis of convergence at diffrent height

    Table  3  The score sheet of severe weather from June to August in2009

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    • Received : 2009-11-16
    • Accepted : 2010-07-08
    • Published : 2010-10-31

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