Zhou Kanghui, Zheng Yongguang, Lan Yu. Flash cell identification, tracking and nowcasting with lightning data. J Appl Meteor Sci, 2016, 27(2): 173-181. DOI:  10.11898/1001-7313.20160205.
Citation: Zhou Kanghui, Zheng Yongguang, Lan Yu. Flash cell identification, tracking and nowcasting with lightning data. J Appl Meteor Sci, 2016, 27(2): 173-181. DOI:  10.11898/1001-7313.20160205.

Flash Cell Identification, Tracking and Nowcasting with Lightning Data

DOI: 10.11898/1001-7313.20160205
  • Received Date: 2015-05-18
  • Rev Recd Date: 2016-01-29
  • Publish Date: 2016-03-31
  • Lightning, accompanying with convective storms in the whole lifecycle, can reflect the development of storms effectively. The national lightning detection network makes it possible to get lightning location data instantly all over China, which would be highly valuable in convective system monitoring. A new method for flash cell identification, tracking and nowcasting is proposed. Using cloud-to-ground lightning location data over China, a new cluster algorithm of fast searching and density peaks identifying, is utilized to recognize the flash cells by clustered flashes. Time and area distribution characteristics of flashes are used in identification. Second, Kalman filtering is used to track the moving path of cells, considering cell spitting and merging conditions. Finally, based on the previous path, the linear moving path in next 60 min is predicted with Kalman filtering.lightning location data in 2013 are analyzed by this method. Doppler radar data are applied to evaluate its performance, which proves its effectiveness on identification and track for thunderstorm split and merge. The overall performance is as better as TITAN (Thunderstorm Identification, Tracking, Analysis and Nowcasting) for thunderstorm nowcasting in 60 minutes, and even better from some aspects. The probability of detection of nowcasting for 10 min is about 0.7, about 0.6 for 30 min and 0.2 for 60 min, respectively. The probability of detection and critical success index decrease dramatically with time, and the false alarm rate increases rapidly in 60 min. All of those mean that the linear nowcasting would be more reliable in near time, and it is meaningful in 0-60 min forecast.One case is analyzed in detail, which shows that flashes only appear in deep convective systems that usually companies with severe weather. Furthermore, flashes disappears obviously in the dissipative stage of storms, which would be an indicator for predicting the end of convective systems.
  • Fig. 1  The clustering algorithm in two dimensions (from refrence[17])

    (point with number is ranked in order of decreasing density, different color corresponds to different cluster) (a) point distribution, (b) decision graph

    Fig. 2  The merge (a) and split (b) of flash cells

    Fig. 3  The process of flash cells identification, track and nowcasting

    Fig. 4  The lightning clusters identification

    (the ellipse denotes the boundary of cluster) (a) the clustered result (the red dot denotes lightning), (b) the clustered result compared with radar echo

    Fig. 5  The lightning distribution and track paths of thunderstorms in South China on 20 Mar 2013

    (the black dash line denotes the tracked path, S is the start symbol, number denotes is the corresponding moment, red point denotes negative flash, blue point denotes positive flash)

    Fig. 6  The track paths of thunderstorms in South China on 20 Mar 2013

    Table  1  The evaluation of nowcasting in 60 minutes

    时间 外推提前时间/min 命中率 漏报率 临界成功指数
    2013-03-19 10 0.69 0.46 0.44
    30 0.64 0.56 0.35
    60 0.18 0.77 0.11
    2013-03-20 10 0.71 0.49 0.42
    30 0.60 0.62 0.30
    60 0.51 0.68 0.24
    1991-05-29—08-29[6] 12 0.64 0.40 0.45
    30 0.42 0.62 0.25
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    • Received : 2015-05-18
    • Accepted : 2016-01-29
    • Published : 2016-03-31

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