Vol.32, NO.3, 2021
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Article Navigation >  Journal of Applied Meteorological Science  > 2021  >  32(3): 358-369
Ma Ruiyang, Zheng Dong, Yao Wen, et al. Thunderstorm feature dataset and characteristics of thunderstorm activities in China. J Appl Meteor Sci, 2021, 32(3): 358-369.DOI:  10.11898/1001-7313.20210308.
Citation: Ma Ruiyang, Zheng Dong, Yao Wen, et al. Thunderstorm feature dataset and characteristics of thunderstorm activities in China. J Appl Meteor Sci, 2021, 32(3): 358-369.DOI:  10.11898/1001-7313.20210308.
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Thunderstorm Feature Dataset and Characteristics of Thunderstorm Activities in China

DOI: 10.11898/1001-7313.20210308

  • Laboratory of Lightning Physics and Protection Engineering/State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081

  • Received Date: 2021-01-12
  • Rev Recd Date: 2021-03-12
  • Publish Date: 2021-05-31
    Abstract
  • A thunderstorm feature dataset (TFD) is built up based on the black body temperature (TBB) product and cloud classification (CLC) product of FY-2E meteorological satellite as well as the lightning data of the World-Wide Lightning Location Network (WWLLN). In the TFD, thunderstorm cloud is determined when there is WWLLN lightning in the area with TBB not higher than -32℃ or its fitted ellipse. The characteristic parameters of thunderstorms including time, location, morphology, structure, and lightning activities are obtained to establish the TFD. Based on the dataset, thunderstorms in the land of China and the adjacent seas are analyzed after the quality control.The results show that South China, Southwest China, Eastern and Central of Tibetan Plateau and South China Sea are the areas with most frequent thunderstorm activities. North China and Northeast China are two areas with relatively frequent thunderstorm activities in the north part of China. Meanwhile, thunderstorm activity is the weakest in Northwest China.The seasonal variation of thunderstorm activity shows obvious differences between land and sea. The active stage of thunderstorms on land is from June to August. In high latitudes, the peak appears earlier. There is a peak of thunderstorm activity in the South China Sea around May, and another peak after August. The lower the latitude is, the later the second peak appears. The peak time of thunderstorm activity in diurnal variation in most parts of the land is from 1400 BT to 2000 BT and the peak of thunderstorm activity in adjacent sea areas mainly occurs in the morning. In the Sichuan Basin, thunderstorms are more frequent in the early morning. The diurnal variation of thunderstorm activity in the South China Sea is relatively weak.The area of thunderstorm cloud with TBB not higher than -32℃ follows a log-normal distribution, with the peak interval being 1×103-1×104 km2, and the average area is 3.0×104 km2. The area of thunderstorm cloud over the sea is obviously larger than that of land, and the South China Sea has the largest area of thunderstorm clouds. On the land, the area of thunderstorm clouds in the east is larger than that in the west, and the average area of thunderstorm clouds greater than 1.2×105 km2 can be predominantly found in the first step of Chinese topography. Meanwhile, there is a local center with an average area of thunderstorm clouds greater than 1.2×105 km2 in the Qaidam Basin.
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    References(34)

  • Fig. 1  Schematic diagram of thunderstorm cloud area identification

    (red lines enclose the areas with TBB not higher than-32℃, blue lines represent the fitted ellipses for these areas, and the yellow * marks superimposed one-hour WWLLN lightning flash;red and blue solid lines represent thunderstorms, and red and blue dashed lines represent non-thunderstorms)

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    Fig. 2  Sample number in lightning frequency(F) and thunderstorm cloud area(A)

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    Fig. 3  Annual thunderstorm hour density during 2010-2018

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    Fig. 4  Annual thunderstorm days in land area of China during 1961-2014

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    Fig. 5  Proportion of ten-day thunderstorm-hour along 30°-32°N and 112°-114°E during 2010-2018

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    Fig. 6  Peak time of thunderstorm activity during 2010-2018

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    Fig. 7  Proportion of thunderstorm-hour along 30°-32°N and 112°-114°E during 2010-2018

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    Fig. 8  Probability and cumulative probability distributions of thunderstorm cloud area(A) in the study area from May to Sep during 2010-2018

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    Fig. 9  Average expansion area of thunderstorm clouds in the study area from May to Sep during 2010-2018

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  • [1]
    Maddox R A.Mesoscale convective complexes.Bull Amer Meteor Soc,1980,61(11):1374-1400. doi:  10.1175/1520-0477(1980)061<1374:MCC>2.0.CO;2
    [2]
    Ma Y, Wang X, Tao Z Y. Census and spatio-temporal distribution characteristics of mesoscale convective systems in China and its adjacent areas. Progress in Natural Science, 1997, 7(6): 701-706. doi:  10.3321/j.issn:1002-008X.1997.06.010
    [3]
    Zheng Y G, Chen J, Zhu P J. Distribution and diurnal variation of summer mesoscale convective system in China and its adjacent areas. Science Bulletin, 2008, 53(4): 471-481. doi:  10.3321/j.issn:0023-074X.2008.04.015
    [4]
    Qi X X, Zheng Y G. Distribution and spatiotemporal variations of deep convection over China and its vicinity during the summer of 2007. J Appl Meteor Sci, 2009, 20(3): 286-294. doi:  10.3969/j.issn.1001-7313.2009.03.004
    [5]
    Su A F, Sun J L, Gu X J, et al. Characteristics and conceptual models of convective rainstorm clouds in Henan Province. J Appl Meteor Sci, 2013, 24(2): 219-229. doi:  10.3969/j.issn.1001-7313.2013.02.010
    [6]
    Yang X, Fei J, Huang X, et al. Characteristics of mesoscale convective systems over China and its vicinity using geostationary satellite FY2. J Climate, 2015, 28(12): 4890-4907. doi:  10.1175/JCLI-D-14-00491.1
    [7]
    Liu C, Zipser E J. Global distribution of convection penetrating the tropical tropopause. J Geophys Res, 2005, 110(23): 1-12. doi:  10.1029/2005JD006063/full
    [8]
    Houze R A, Wilton D C, Smull B F. Monsoon convection in the Himalayan region as seen by the TRMM Precipitation Radar. Quart J Roy Meteor Soc, 2007, 133: 1389-1411. http://ci.nii.ac.jp/naid/10025262410
    [9]
    Romatschke U, Medina S, Houze R A. Regional, seasonal, and diurnal variations of extreme convection in the South Asian region. J Climate, 2010, 23(2): 419-439. doi:  10.1175/2009JCLI3140.1
    [10]
    Wu X K, Qie X S, Yuan T. Regional distribution and diurnal variation of deep convective systems over the Asian monsoon region. Science China(Earth Sciences), 2013, 56(5): 843-854. doi:  10.1007/s11430-012-4551-8
    [11]
    Qie X, Wu X, Yuan T, et al. Comprehensive pattern of deep convective systems over the Tibetan Plateau-South Asian monsoon region based on TRMM data. J Climate, 2014, 27(17): 6612-6626. doi:  10.1175/JCLI-D-14-00076.1
    [12]
    Zhu S C, Yuan Y, Wu Y, et al. Statistical characteristics of isolated convection in the Jianghuai Region. J Appl Meteor Sci, 2019, 30(6): 690-699. doi:  10.11898/1001-7313.20190605
    [13]
    Mezuman K, Price C, Galanti E. On the spatial and temporal distribution of global thunderstorm cells. Environ Res Lett, 2014, 9(12). DOI: 10.1088/1748-9326/9/12/124023.
    [14]
    Hutchins M L, Holzworth R H, Brundell J B. Diurnal variation of the global electric circuit from clustered thunderstorms. J Geophys Res(Space Physics), 2014, 119(1): 620-629. doi:  10.1002/2013JA019593/full
    [15]
    Zhou K H, Zheng Y G, Lan Y. Flash cell identification, tracking and nowcasting with lightning data. J Appl Meteor Sci, 2016, 27(2): 173-181. doi:  10.11898/1001-7313.20160205
    [16]
    Liu C, Zipser E J, Cecil D J, et al. A cloud and precipitation feature database from nine years of TRMM observations. J Appl Meteor Climatol, 2008, 47(10): 2712-2728. doi:  10.1175/2008JAMC1890.1
    [17]
    Zipser E J, Cecil D J, Liu C, et al. Where are the most: Intense thunderstorms on Earth?. Bull Amer Meteor Soc, 2006, 87(8): 1057-1071. doi:  10.1175/BAMS-87-8-1057
    [18]
    Bang S D, Zipser E J. Differences in size spectra of electrified storms over land and ocean. Geophys Res Lett, 2015, 42: 6844-6851. doi:  10.1002/2015GL065264
    [19]
    Bang S D, Zipser E J. Seeking reasons for the differences in size spectra of electrified storms over land and ocean. J Geophys Res, 2016, 121(15): 9048-9068. doi:  10.1002/2016JD025150
    [20]
    Li J L, Wu X K, Yuan T, et al. The temporal and spatial distribution of thunderstorms in Asia Monsoon region based on the TRMM multi-sensor database. Chinese J Geophys, 2019, 62(11): 4098-4109. doi:  10.6038/cjg2019M0687
    [21]
    Dowden R L, Brunde J B, Rodger C J. VLF lightning location by time of group arrival (TOGA) at multiple sites. J Atmos Solar-Terr Phys, 2002, 64(7): 817-830. doi:  10.1016/S1364-6826(02)00085-8
    [22]
    Dowden R L, Holzworth R H, Rodger C J, et al. World-wide lightning location using VLF propagation in the Earth-ionosphere waveguide. IEEE Antenn Propag M, 2008, 50(5): 40-60. doi:  10.1109/MAP.2008.4674710
    [23]
    Hutchins M L, Holzworth R H, Brundell J B, et al. Relative detection efficiency of the World Wide Lightning Location Network. Radio Sci, 2012, 47(6): 1-9. http://ieeexplore.ieee.org/document/7776718
    [24]
    Rudlosky S D, Shea D T. Evaluating WWLLN performance relative to TRMM/LIS. Geophys Res Lett, 2013, 40(10): 2344-2348. doi:  10.1002/grl.50428
    [25]
    Bürgesser R E. Assessment of the World Wide Lightning Location Network (WWLLN) detection efficiency by comparison to the Lightning Imaging Sensor (LIS). Quarty J Roy Meteor Soc, 2017, 143(708): 2809-2817. doi:  10.1002/qj.3129
    [26]
    Fan P, Zheng D, Zhang Y, et al. A Performance evaluation of the World Wide Lightning Location Network (WWLLN) over the Tibetan Plateau. J Atmos Ocean Technol, 2018, 35(4): 927-939. doi:  10.1175/JTECH-D-17-0144.1
    [27]
    Boccippio D J, Koshak W J, Blakeslee R J. Performance assessment of the optical transient detector and lightning imaging sensor. Part Ⅰ: Predicted diurnal variability. J Atmos Ocean Technol, 2002, 19(9): 1318-1332. doi:  10.1175/1520-0426(2002)019<1318:PAOTOT>2.0.CO;2
    [28]
    Fei Z P, Wang H Q, Zheng Y G, et al. MCS census and modification of MCS definition based on geostationary satellite infrared imagery. J Appl Meteor Sci, 2008, 19(1): 82-90. doi:  10.3969/j.issn.1001-7313.2008.01.011
    [29]
    Cao Z Q, Wang X. Cloud characteristics and synoptic background associated with severe convective storms. J Appl Meteor Sci, 2013, 24(3): 365-372. doi:  10.3969/j.issn.1001-7313.2013.03.013
    [30]
    Wang X, Guo Q, Chen Y Y. Performance improvement for FY-2E convection monitoring using a spatial-response matched filter method. J Appl Meteor Sci, 201627(1): 102-111. doi:  10.11898/1001-7313.20160111
    [31]
    Feng J Q, Liu M, Cai J. Meso-scale convective characteristics of "7·22" extreme rain in the west mountainous area of Fujian. J Appl Meteor Sci, 2018, 29(6): 748-758. doi:  10.11898/1001-7313.20180610
    [32]
    Thiel K C, Calhoun K M, Reinhart A E, et al. GLM and ABI characteristics of severe and convective storms. J Geophys Res Atmos, 2020, 125(17): 1-22. doi:  10.1029/2020JD032858
    [33]
    Jin X, Study of Diurnal Cycle of Precipitation over the Sichuan Basin: Characteristics and its Causes. Beijing: Chinese Academy of Meteorological Sciences, 2013.
    [34]
    Wang H, Li Y, Song L L, et al. Comparison of characteristics and environmental factors of thunderstorm gales over the Sichuan-Tibet Region. J Appl Meteor Sci, 2020, 31(4): 435-446. doi:  10.11898/1001-7313.20200406
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    • Received : 2021-01-12
    • Accepted : 2021-03-12
    • Published : 2021-05-31
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