Tian Ye, Yao Wen, Yin Jiali, et al. Comparison of the performance of different lightning jump algorithms in Beijing. J Appl Meteor Sci, 2021, 32(2): 217-232. DOI:  10.11898/1001-7313.20210207.
Citation: Tian Ye, Yao Wen, Yin Jiali, et al. Comparison of the performance of different lightning jump algorithms in Beijing. J Appl Meteor Sci, 2021, 32(2): 217-232. DOI:  10.11898/1001-7313.20210207.

Comparison of the Performance of Different Lightning Jump Algorithms in Beijing

DOI: 10.11898/1001-7313.20210207
  • Received Date: 2020-09-29
  • Rev Recd Date: 2020-12-23
  • Publish Date: 2021-03-31
  • Based on S-band Doppler weather radar raw data, the total lightning location data of Beijing Lightning Network (BLNET) and hailfall reports from Beijing Meteorological Service, two lightning jump algorithms, Gatlin algorithm and σ algorithm, with different configurations are compared and analyzed for early warning performance of 177 hailfall events in Beijing from 2015 to 2018. The results show that, the early warnings of different multiples of σ algorithm are quite different, 2σ (in this situation, the current changing rate of total flash exceeds two times of the standard deviation of total flash rate in previous time) has the best performance in the σ algorithm. That is to say, 2σ algorithm has the highest probability of detection (POD) and critical success index (CSI), as well as the lowest false alarm rate (FAR), comparing with σ, 3σ and 4σ algorithms. The early warnings of Gatlin algorithm under different N (which is the amount of samples before current time used to calculate the mean and standard deviation) configurations have little difference, and the early warning efficiency is best when N=6, comparing with N=7, 8, 9 and 10. The POD, FAR and CSI of 2σ algorithm are 80.2%, 41.6%, and 51.1%, respectively. The corresponding results of the Gatlin algorithm with N=6 are 82.5%, 62.0%, and 35.2%, respectively. In addition, the applications of these two algorithms to a multi-cell thunderstorm process and a squall line process are analyzed in detail. The results also show that Gatlin algorithm with N=6 has a slightly higher POD than 2σ algorithm, but its FAR is much higher and its CSI is lower. Considering the evaluation of hail nowcast results by Gatlin algorithm and 2σ algorithm, 2σ lightning jump algorithm is more suitable for hail nowcasting in Beijing. And it is beneficial to improving the application of lightning data to hail nowcasting in Beijing
  • Fig. 1  Distribution map of BLNET stations

    Fig. 2  Comparison of early warning effects of different σ thresholds

    Fig. 3  Comparison of the early warning effects of Gatlin algorithm with different N of D

    Fig. 4  Radar composite reflectivity of a multi-cell convective system across Beijing on 8 Aug 2017

    (the black six-pointed star indicates the hailfall position)

    Fig. 5  Identification results of strong convection cells on 8 Aug 2017

    (the red polygon marks the hail-producing convection cell, the black six-pointed star indicates the hailfall position)

    Fig. 6  Identified strong convection cells and the located total flashes in 3 min before and after the corresponding time

    (the red dot indicates the intracloud flash, the red × indicates the negative cloud-to-ground flash and the red + indicates the positive cloud-to-ground flash, the black six-pointed star indicates the hailfall position, the illustration is an enlarged view of superposition of the split cell and the total flashes in the figure of 1948 BT)

    Fig. 7  The lightning flash rate of the hail-producing cell of the multi-cell system and total flash rates(the columns) and jump thresholds(the pink curves) derived by 2σ algorithm and Gatlin algorithm

    Fig. 8  Radar composite reflectivity of a squall line across Beijing on 7 Aug 2015

    (the black six-pointed star indicates the hailfall position, the number in each subgraph indicates the sequence of the hailfall events)

    Fig. 9  Identification results of every strong convection cells during the squall line process

    (the black six-pointed star indicates the hailfall position, the number indicates the sequence of the hailfall events)

    Fig. 10  The lightning flash rate of the haill-producing cell of the squall line system and total flash rates(the columns) and jump thresholds(the pink curves) derived by 2σ algorithm and Gatlin algorithm

    Table  1  The lightning jump information of 2σ algorithm for a squall line process in Beijing on 7 Aug 2015

    跃增时刻 降雹时刻 与首次跃增时刻相比得到的预警提前时间/min
    16:42,16:48 17:40—17:41 58
    17:10,17:16,17:26,17:28,17:40 18:00—18:06 50
    18:28 18:50—18:53 22
    18:28,18:30,18:52 19:15—19:20 47
    18:28,18:30,18:52 19:16—19:17 48
    19:58—20:01 漏报
    DownLoad: Download CSV

    Table  2  The lightning jump information of Gatlin algorithm for a squall line process in Beijing on 7 Aug 2015

    跃增时刻 降雹时刻 与首次跃增时刻相比得到的预警提前时间/min
    16:42,16:48,16:54 17:40—17:41 58
    17:00,17:06,17:10,17:16,17:26,17:28,17:34,17:40,17:42 18:00—18:06 60
    18:28,18:30,18:32,18:52 18:50—18:53 22
    18:56,19:16 19:15—19:20 19
    18:56,19:16 19:16—19:17 20
    19:28,19:36 19:58—20:01 30
    DownLoad: Download CSV
  • [1]
    Wang T B, Zheng D, Zhou K H, et al. Contrastive analysis of lightning characteristics between rainstorm case and hailstorm case. J Appl Meteor Sci, 2017, 28(5): 568-578. doi:  10.11898/1001-7313.20170505
    [2]
    Goodman S J, Christian H J, Rust W D. A comparison of the optical pulse characteristics of intracloud and cloud-to-ground lightning as observed above clouds. J Appl Meteorol, 1988, 27(12): 1369-1381. doi:  10.1175/1520-0450(1988)027<1369:ACOTOP>2.0.CO;2
    [3]
    Lang T J, Rutledge S A.One Severe Storm with Two Distinct Electrical Regimes During its Lifetime: Implications for Nowcasting Severe Weather with Lightning Data//Proceedings of 1st Conference of Meteorological Applications of Lightning Data, San Diego, CA, 2005.
    [4]
    McKinney C M, Carey L D, Patrick G R. Total lightning observations of supercells over north central Texas. Electronic J Severe Storms Meteor, 2009, 4(2): 1-25. http://search.ebscohost.com/login.aspx?direct=true&db=aph&AN=52225677&site=ehost-live
    [5]
    Darden C B, Nadler D J, Carcione B C, et al. Utilizing total lightning information to diagnose convective trends. Bull Amer Meteor Soc, 2010, 91(2): 167-175. doi:  10.1175/2009BAMS2808.1
    [6]
    Rudlosky S D, Fuelberg H E. Documenting storm severity in the mid-Atlantic region using lightning and radar information. Mon Wea Rev, 2013, 141(9): 3186-3202. doi:  10.1175/MWR-D-12-00287.1
    [7]
    Zhu J J, Diao X G, Huang X S. Study of CINRAD/SA products for a hail storm. J Appl Meteor Sci, 2004, 15(5): 579-589. http://qikan.camscma.cn/article/id/20040571
    [8]
    Wang J, Liu L P. The evaluation of WSR-88D hail detection algorithm over Guizhou region. J Appl Meteor Sci, 2011, 22(1): 96-106. http://qikan.camscma.cn/article/id/20110110
    [9]
    Zhang B X, Li G C, Liu L P, et al. Identification method of hail weather based on fuzzy-logical principle. J Appl Meteor Sci, 2014, 25(4): 415-426. http://qikan.camscma.cn/article/id/20140404
    [10]
    Shi B L, Wang H Y, Liu L P. Coverage capacity of hail detection for Yunnan doppler weather radar network. J Appl Meteor Sci, 2018, 29(3): 270-281. doi:  10.11898/1001-7313.20180302
    [11]
    Kane R J. Correlating lightning to severe local storms in the northeastern United States. Wea Forecasting, 1991, 6(1): 3-12. doi:  10.1175/1520-0434(1991)006<0003:CLTSLS>2.0.CO;2
    [12]
    Williams E R, Boldi B, Matlin A, et al. The behavior of total lightning activity in severe Florida thunderstorms. Atmos Res, 1999, 51(3/4): 245-265. http://www.sciencedirect.com/science/article/pii/S0169809599000113
    [13]
    Metzger E, Nuss W A. The relationship between total cloud lightning behavior and radar-derived thunderstorm structure. Wea Forecasting, 2010, 28(1): 237-253. http://adsabs.harvard.edu/abs/2013WtFor..28..237M
    [14]
    Goodman S J, Blakeslee T R, Christian H, et al. The North Alabama lightning mapping array: Recent severe storm observations and future prospects. Atmos Res, 2005, 76(1/2/3/4): 423-437. http://www.sciencedirect.com/science/article/pii/S0169809505000645
    [15]
    Schultz C J, Petersen W A, Carey L D. Preliminary development and evaluation of lightning jump algorithms for the real-time detection of severe weather. J Appl Meteorol Climatol, 2009, 48(12): 2543-2563. doi:  10.1175/2009JAMC2237.1
    [16]
    Wapler K. The life-cycle of hailstorms: Lightning, radar reflectivity and rotation characteristics. Atmos Res, 2017, 193: 60-72. doi:  10.1016/j.atmosres.2017.04.009
    [17]
    Chen Z Z. The characteristics of lightning from clouds to ground accompanying with hailstones, thunderstorms and gusts. Acta Meteor Sinica, 1995, 53(3): 367-374. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXB503.012.htm
    [18]
    Zhou Y J, Zhang Y J, Qie X S, et al. The relationship between the variation of hail cloud system and its cloud to ground lightning in the east part of Gansu province. Plateau Meteor, 1999, 18(2): 236-244. https://www.cnki.com.cn/Article/CJFDTOTAL-GYQX902.012.htm
    [19]
    Cai X Y, Wan X, Guo H. Application analysis of lightning location data in Beijing area. Meteor Sci Technol, 2001, 29(4): 33-35. https://www.cnki.com.cn/Article/CJFDTOTAL-QXKJ200104007.htm
    [20]
    Feng G L, Bian D X, Liu H P, et al. The evolution of hail cloud system and characterof its cloud to ground lightning. Meteor Mon, 2001, 27(3): 33-37. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200103008.htm
    [21]
    Feng G L, Qie X S, Yuan T, et al. A case study of cloud-to-ground lightning activities in hailstorms under cold eddy synoptic situation. Acta Meteor Sinica, 2006, 64(2): 85-94. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200602008.htm
    [22]
    Feng G L, Qie X S, Wu S J. Cloud-to-ground lightning characteristics of hail clouds in Shandong province. Chin J Atmos Sci, 2008, 32(2): 289-299. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200802007.htm
    [23]
    Liu D, Feng G, Wu S. The characteristics of cloud-to-ground lightning activity in hailstorms over northern China. Atmos Res, 2009, 91(2-4): 459-465. http://www.sciencedirect.com/science/article/pii/S0169809508002196
    [24]
    Gatlin P N.Severe Weather Precursors in the Lightning Activity of Tennessee Valley Thunderstorms.Department of Atmospheric Sciences, University of Alabama, 2007.
    [25]
    Schultz C J, Petersen W A, Carey L D. Lightning and severe weather: A comparison between total and cloud-to-ground lightning trends. Wea Forecasting, 2011, 26(5): 744-755. http://adsabs.harvard.edu/abs/2011WtFor..26..744S
    [26]
    Yao W, Zhang Y, Meng Q, et al. A comparison of the characteristics of total and cloud-to-ground lightning activities in hailstorms. Acta Meteor Sinica, 2013, 27(2): 282-293. http://www.cnki.com.cn/Article/CJFDTotal-QXXW201302013.htm
    [27]
    Chronis T, Carey L D, Schultz C J, et al. Exploring lightning jump characteristics. Wea Forecasting, 2015, 30(1): 23-37. http://adsabs.harvard.edu/abs/2015WtFor..30...23C
    [28]
    Tian Y, Qie X S, Sun Y, et al. Total lightning signatures of thunderstorms and lightning jumps in hailfall nowcasting in the Beijing area. Atmos Res, 2019, 230: 104646. http://www.sciencedirect.com/science/article/pii/S0169809519309020
    [29]
    Zhang W J, Meng Q, Lü W T, et al. Error analyses and network optimization for time-of-arrival lightning locating system. J Appl Meteor Sci, 2009, 20(4): 402-410. http://qikan.camscma.cn/article/id/20090403
    [30]
    Wang Y, Qie X S, Wang D F, et al. Beijing lightning network (BLNET) and the observation on preliminary breakdown processes. Atmos Res, 2016, 171: 121-132. http://www.sciencedirect.com/science/article/pii/S0169809515004020
    [31]
    Srivastava A, Tian Y, Qie X S, et al. Performance assessment of Beijing Lightning Network (BLNET) and comparison with other lightning location networks across Beijing. Atmos Res, 2017, 197: 76-83. http://www.sciencedirect.com/science/article/pii/S016980951730217X
    [32]
    Dixon M, Wiener G. TITAN: Thunderstorm identification, tracking, analysis, and nowcasting-A radar-based methodology. J Atmos Ocean Technol, 1993, 10(10): 785-797. http://ci.nii.ac.jp/naid/80007371603
    [33]
    Schultz C J, Carey L D, Schultz E V, et al. Kinematic and microphysical significance of lightning jumps versus nonjump increases in total flash rate. Wea Forecasting, 2017, 32(1): 275-288. http://europepmc.org/abstract/MED/29158622
    [34]
    Gatlin P N, Goodman S J. A total lightning trending algorithm to identify severe thunderstorms. J Atmos Ocean Technol, 2010, 27(1): 3-22. http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010JAtOT..27....3G&db_key=PHY&link_type=ABSTRACT
    [35]
    Lan Y, Zheng Y G, Mao D Y, et al. Classification and satellite nephogram features of hail weather in North China. J Appl Meteor Sci, 2014, 25(5): 538-549. http://qikan.camscma.cn/article/id/20140503
    [36]
    Xu S, Zheng D, Wang Y, et al. Characteristics of the two active stages of lightning activity in two hailstorms. J Meteor Res, 2016, 30(2): 265-281. http://www.cqvip.com/QK/88418X/20162/668824630.html
    [37]
    Hu S, Luo C, Zhang Y, et al. Doppler radar features of severe hailstorms in Guangdong Province. J Appl Meteor Sci, 2015, 26(1): 57-65. doi:  10.11898/1001-7313.20150106
    [38]
    Liu Z, Guo F X, Zheng D, et al. Lightning activities in a convection cell dominated by heavy warm cloud precipitation. J Appl Meteor Sci, 2020, 31(2): 185-196. doi:  10.11898/1001-7313.20200206
  • 加载中
  • -->

Catalog

    Figures(10)  / Tables(2)

    Article views (1693) PDF downloads(135) Cited by()
    • Received : 2020-09-29
    • Accepted : 2020-12-23
    • Published : 2021-03-31

    /

    DownLoad:  Full-Size Img  PowerPoint