Liu Xiaolu, Liu Jianxi, Zhang Shilin, et al. Hail forecast based on factor combination analysis method and sounding data. J Appl Meteor Sci, 2014, 25(2): 168-175.
Citation: Liu Xiaolu, Liu Jianxi, Zhang Shilin, et al. Hail forecast based on factor combination analysis method and sounding data. J Appl Meteor Sci, 2014, 25(2): 168-175.

Hail Forecast Based on Factor Combination Analysis Method and Sounding Data

  • Received Date: 2013-05-07
  • Rev Recd Date: 2013-11-20
  • Publish Date: 2014-03-31
  • The emergence of the small probability of severe weather events is attributed to specific factor combinations of some early meteorological elements. The nonlinear and complicated characteristics of factor combinations can be used to find the relationship between forecast object and forecast factors. Based on this method, the relationship between hail events in the south of Sichuan Basin and some meteorological elements calculated by the sounding data is investigated, and a hail forecast index discriminant is established. The discriminant is physically significant and applied in daily operation.Hailstorm is a meso-scale weather system with the temporal scale of several to dozens of hours, and the horizontal scale of several hundred kilometers. In real business, the T-lnp sounding data are observed at 0800 BT and 2000 BT every day, and the hail forecasting is carried out every 12 hours. A sample sets of 7 hail events and 38 non-hail events near Yibin Station is established. Using the T-lnp sounding data, 3422 meteorological elements are calculated as forecast factors, including temperature, height, moisture, saturation vapor pressure, potential pseudo-equivalent temperature, K index and so on. Based on factors combination analysis method, 2 main factors and 2 conditional factors are selected from 3422 meteorological elements and their critical values are calculated. The main factors are Tσ400*-Tσ850 and Gz400-Gzsurface, and the conditional factors are e700-es700 and Td700-Tσ700*, Tσ400* stands for saturated wet static temperature at 400 hPa, and Tσ850 stands for wet static temperature at 850 hPa; Gz400 and Gzsurface stand for vertical pressure gradient at 400 hPa and the surface level; e700 and es700 stand for vapour pressure and saturated vapour pressure at 700 hPa; Td700 and Tσ700* stand for dew point temperature and saturated wet static temperature at 700 hPa. The hail forecast indexes discriminant nearby Yibin Station is established using these data.The environmental state of hailstorm generation and the unstable mechanism of severe convective weather can be explained by the hail forecast indexes discriminant, which is evaluated using historical records of the year of 2008. Among 65 warnings, the real hail events never miss but the false alarm ratio reaches 67.7%, which should be further distinguished using radar observations. The overall probability of detection is 84%, and the critical success index is 30.4%. The result shows that factor combination analysis method is feasible to some extent.
  • Table  1  Hail event samples

    序号 探空资料时间 降雹时间 降雹地点 降雹地与探空站距离/km 降雹地海拔/m 冰雹直径/mm
    1 1983-04-10T20:00 22:47 宜宾 0 341 5
    2 1985-08-06T08:00 17:57 荣县 72 382 20
    3 1994-07-18T08:00 16:45 隆昌 88 374 9
    4 1994-07-27T08:00 15:12 井研 106 419 8
    5 1998-04-28T08:00 18:42 珙县 48 368 14
    6 2000-07-20T08:00 17:18 井研 106 419 20
    7 2002-04-04T08:00 18:50 自贡 61 357 8
    DownLoad: Download CSV

    Table  2  Sequence Y and sequence of top 10 major factors

    样本YX1X2X3X4X5X6X7X8X9X10
    111111111111
    211111111111
    311111111111
    411111111111
    511111111111
    611111111111
    711111111111
    801011111111
    901111111111
    1000000000000
    1100000000000
    1200000000000
    1300000000000
    1400000000000
    1500000000000
    1601111111111
    1700011001111
    1800000000000
    1900000000000
    2000000000000
    2100000000000
    2200000000000
    2300000000000
    2400000000000
    2500001001111
    2601111111111
    2701100110000
    2800000000000
    2900000000000
    3000000000000
    3100000000000
    3200000000000
    3300000000000
    3400000000000
    3500111111111
    3600111111111
    3700000001111
    3800000000000
    3900000000000
    4000010110000
    4101011111111
    4201111111111
    4300101111111
    4400110000000
    4500101111111
    DownLoad: Download CSV

    Table  3  Sequence of major factor combination and its top 8 condition factors

    样本YV1∧2YYX1X2X3X4X5X6X7X8
    1110111111110
    2110110000000
    3110111111111
    4110111111100
    5110111111111
    6110111100001
    7110101111111
    8000100101010
    9011000000000
    10000111111110
    11000111111111
    12000111111111
    13000111111111
    14000111111111
    15000111111111
    16011000000000
    17000111111101
    18000111101110
    19000111111110
    20000111111111
    21000111111110
    22000111111110
    23000111111111
    24000111111111
    25000100001011
    26011000000000
    27011000000000
    28000111111111
    29000111101101
    30000111111111
    31000111111111
    32000101111111
    33000100011110
    34000100000001
    35000111111101
    36000111100101
    37000111111101
    38000111111111
    39000100000101
    40000100011111
    41000100000000
    42011000000000
    43000111111101
    44000111111110
    45000101110100
    DownLoad: Download CSV
  • [1]
    何立富, 周庆亮, 谌芸, 等.国家级强对流潜势预报业务进展与检验评估.气象, 2011, 37(7):777-784. doi:  10.7519/j.issn.1000-0526.2011.07.001
    [2]
    彭治班, 刘健文, 郭虎, 等.国外强对流天气的应用研究.北京:气象出版社, 2001.
    [3]
    王笑芳, 丁一汇.北京地区强对流天气短时预报方法的研究.大气科学, 1994, 18(2):173-183. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK199402004.htm
    [4]
    李耀东, 高守亭, 刘健文.对流能量计算及强对流天气落区预报技术研究.应用气象学报, 2004, 15(1):10-20. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040102&flag=1
    [5]
    李耀东, 刘健文, 高守亭.动力和能量参数在强对流天气预报中的应用研究.气象学报, 2004, 62(4):401-409. doi:  10.11676/qxxb2004.041
    [6]
    廖晓农, 俞小鼎, 于波.北京盛夏一次罕见的大雹事件分析.气象, 2008, 34(2):10-17. doi:  10.7519/j.issn.1000-0526.2008.02.002
    [7]
    雷蕾, 孙继松, 魏东.利用探空资料判别北京地区夏季强对流的天气类别.气象, 2011, 37(2):136-141. doi:  10.7519/j.issn.1000-0526.2011.02.002
    [8]
    高宾永, 杨仕贤, 吴海涛, 等.运用能量学方法分析大冰雹的落区.气象与环境科学, 2010, 33(2):68-71. http://www.cnki.com.cn/Article/CJFDTOTAL-HNQX201002014.htm
    [9]
    陈晓红, 郝莹, 周后福, 等.一次罕见冰雹天气过程的对流参数分析.气象科学, 2007, 27(3):335-341. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKX200703017.htm
    [10]
    刘玉玲.对流参数在强对流天气潜势预测中的作用.气象科技, 2003, 31(3):147-151. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKJ200303003.htm
    [11]
    周洪祥.灾害性天气的预测方法.北京:气象出版社, 2002.
    [12]
    Orlanski I.A rational subdivision of scales for atmospheric processes.Bull Amer Meteor Soc, 1975, 56:527-530. http://ci.nii.ac.jp/naid/10003560833/ja/
    [13]
    叶爱芬, 伍志方, 肖伟军, 等.对流有效位能在强对流预报中的应用研究.热带气象学报, 2006, 22(5):484-490. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200605011.htm
    [14]
    雷雨顺.能量天气学.北京:气象出版社, 1986.
    [15]
    陆汉城.中尺度天气原理和预报.北京:气象出版社, 2000.
    [16]
    盛裴轩, 毛节泰, 李建国, 等.大气物理学.北京:北京大学出版社, 2003.
    [17]
    张杰.中小尺度天气学.北京:气象出版社, 2006.
    [18]
    孙继松, 陶祖钰.强对流天气分析与预报中的若干基本问题.气象, 2012, 38(2):164-173. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX201202007.htm
    [19]
    罗阳, 赵伟, 翟景秋.两类天气预报评分问题研究及一种新评分方法.应用气象学报, 2009, 20(2):129-136. doi:  10.11898/1001-7313.20090201
    [20]
    Donaldson R J, Dyer R M, Krauss M J.An Objective Evaluator of Techniques for Predicting Severe Weather Events.9th Conf Severe Local Storms, Amer Meteor Soc, 1975:321-326.
    [21]
    王丽荣, 卞韬, 苏运涛, 等.晴空回波在强对流天气临近预报中的应用.应用气象学报, 2010, 21(5):606-613. doi:  10.11898/1001-7313.20100510
    [22]
    邓国, 龚建东, 邓莲堂, 等.国家级区域集合预报系统研发和性能检验.应用气象学报, 2010, 21(5):513-523. doi:  10.11898/1001-7313.20100501
    [23]
    王瑾, 刘黎平.WSR-88D冰雹探测算法在贵州地区的评估检验.应用气象学报, 2011, 22(1):96-106. doi:  10.11898/1001-7313.20110110
    [24]
    刘春文, 林永辉, 曹艳察.局地分析预报系统在GRAPES模式中的应用.应用气象学报, 2013, 24(2):162-170. doi:  10.11898/1001-7313.20130204
    [25]
    陈明轩, 俞小鼎, 谭晓光, 等.对流天气临近预报技术的发展与研究进展.应用气象学报, 2004, 15(6):754-766. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040693&flag=1
    [26]
    廖晓农, 俞小鼎, 谭一洲.14时探空在改进北京地区对流天气潜势预报中的作用.气象, 2007, 33(3):28-32. doi:  10.7519/j.issn.1000-0526.2007.03.004
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    • Received : 2013-05-07
    • Accepted : 2013-11-20
    • Published : 2014-03-31

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