YUAN Chao,YANG Wenyan,WANG Shigong,et al.Spatial and Temporal Characteristics of Tornadoes in Liaoning Province from 1955 to 2019[J].Journal of Chengdu University of Information Technology,2022,37(04):470-477.[doi:10.16836/j.cnki.jcuit.2022.04.017]
1955-2019年辽宁龙卷时空分布特征
- Title:
- Spatial and Temporal Characteristics of Tornadoes in Liaoning Province from 1955 to 2019
- 文章编号:
- 2096-1618(2022)04-0470-08
- Keywords:
- meteorology; severe weather forecast; tornadoes; spatial-temporal characteristics; disaster feature; Liaoning
- 分类号:
- P468
- 文献标志码:
- A
- 摘要:
- 为研究辽宁地区龙卷气候特征,基于《中国气象灾害大典》《中国气象灾害年鉴》和其他相关资料,采用“改进藤田分级”标准进行强度分类,对1955-2019年辽宁龙卷的时空分布特征进行统计分析,得到以下主要结论:(1)1955-2019年辽宁地区平均每年出现龙卷2.3个,年龙卷密度为1.5×10-5个/km2,约为美国的1/10。EF2及以上等级强龙卷共记录到25次,年均0.4次,含EF4级1次,EF3级3次,EF2级21次,相邻分级比例在0.1~0.36。(2)龙卷主要出现在5-10月,其中7月最多,超过年总数的1/4。龙卷大多出现在午后到傍晚,13-14时、17-18时是两个龙卷多发时段。约85%的龙卷事件持续时间在20分钟以内。(3)多数龙卷发生在平原地区,5-6月多分布于辽西走廊至辽宁西北部地区; 7-8月集中于辽西走廊和辽河平原中下游地区; 9-10月辽宁东部地区龙卷明显增多。
- Abstract:
- In order to study the characteristics of tornadoes in Liaoning province, based on “the Handbook of China Meteorological Disasters”,and“the Annual Report of China Meteorological Disasters” and other related data,the intensity classification was carried out by using the standard of improved Fujita Classification,the temporal and spatial distribution characteristics of tornadoes in Liaoning from 1955 to 2019 were statistically analyzed. Given the study results,(1)From 1955 to 2019,there is a mean of 2.3 tornadoes annually in Liaoning, meanwhile,the annual average tornado density is 1.5×10-5/km2,which is about 1/10 of that in the United States. There is a total of 25 significant tornadoes of EF2 and above were recorded,with an average annual occurrence of 0.4,including one time of grade EF4,3 times of grade EF3,and 21 times of grade EF2.The ratio of adjacent grading is within the range of 0.1-0.36.(2)Tornadoes occur with a maximum from May through October and more than a quarter of the annual total occurred in July.Tornadoes mostly occur in the afternoon to the evening.13:00-14:00 and 17:00-18:00 are two frequent periods of tornadoes.Approximately 85% of tornado events last within 20 minutes.(3)Most tornadoes occur in the plains, while tornadoes are distributed from the Liaoxi Corridor to northwestern Liaoning area from May to June,in the Liaoxi Corridor and the middle and lower reaches of the Liaohe Plain from July to August and increased significantly in the eastern coastal area of Liaoning from September to October.
参考文献/References:
[1] Davies Jones R,Trapp R J,Bluestein H B. Tornadoes and Tornadic Storms[J]. Meteorological Monographs, 2001, 28(50):167-221.
[2] HUANG Dapeng,GAO Ge,YE Dianxiu,et al.Progress in tornado research and present situation of tornado warning operational system[J].Science & Technology Review,2017,35(5):45-53.
[3] ZHANG Xuefen,DU Bo,TANG Zhiya,et al.Spatio-Temporal Distribution of Weather Phenomena in China[J].Meteorological Monthly,2013,39(11):1452-1460.
[4] Fujita T T.Proposed characterization of tornadoes and hurricanes by area and intensity[R].SMRP Research Paper,Chicago:The University of Chicago,1971.
[5] Doswell C A.A guide to F-scale damage assessment.NOAA/NWS[EB/OL].https://training.weather.gov/wdtd/courses/EF-scale/lesson2/FinalNWSF-scaleAssessmentGuide,2003.
[6] Wind Science and Engineering Center.A recommendation for an enhance Fujita scale(EF-scale)[EB/OL].Wind Science and Engineering Center Rep,Texas Tech University, Lubbock,TX.http://www.spc.noaa.gov/faq/tornado/ef-tuu,2004.
[7] Wang Donghai,Li Zhaohui,Gao Zongting,et al.A Comparison of Statistical Characteristics and Research Progress of Tornadoes in China to that in Europe and USA[J].Advances in Meteorological Science and Technology,2018,8(2):8-23.
[8] China Meteorological Administration.Tornado intensity level:QX/T 478-2019[S].Beijing:China Meteorological Press,2019:1-4.
[9] Wei Wenxiu,Zhao Yamin.Several characteristics of tornadoes in China[J].Meteorological Monthly,1995,21(5):37-40.
[10] Yao Y,Yu X,Zhang Y,et al.Climate analysis of tornadoes in China[J].Journal of Meteorological Research,2015.
[11] China Meteorological Bureau.China Meteorological Disaster Yearbook(2005-2013)[M]. Beijing:Meteorological Publishing House,2013.
[12] Fan Wenjie,Yu Xiaoding.Characteristics of spatial-temporal distribution of tornadoes in China[J].Meteorological Monthly,2015,41(7):793-805.
[13] Brooks H E,Lee J W,Craven J P.The spatial distribution of severe thunderstorm and tornado environments from global reanalysis data[J].Atmospheric Research,2003:67-94.
[14] Doswell,Charles A.On Some Issues of United States Tornado Climatology[J].Mon.wea.rev,1988,116(2):495-501.
[15] Agee,Ernest,Childs,et al.Spatial Redistribution of US Tornado Activity between 1954 and 2013[J].Journal of Applied Meteorology & Climatology,2016,55(8).
相似文献/References:
[1]廖洪涛,肖天贵,魏 微,等.东亚梅雨季低频波波包传播特征[J].成都信息工程大学学报,2019,(02):143.[doi:10.16836/j.cnki.jcuit.2019.02.008]
LIAO Hongtao,XIAO Tiangui,WEI Wei,et al.Low Frequency Wave Packet Propagation
Characteristics in East Asian Meiyu Season[J].Journal of Chengdu University of Information Technology,2019,(04):143.[doi:10.16836/j.cnki.jcuit.2019.02.008]
[2]王雨歌,郑佳锋,朱克云,等.一次西南涡过程的云-降水毫米波云雷达回波特征分析[J].成都信息工程大学学报,2019,(02):172.[doi:10.16836/j.cnki.jcuit.2019.02.011]
WANG Yuge,ZHENG Jiafeng,ZHU Keyun,et al.Analysis of Cloud-Precipitation Echo Characteristics of a Southwest Vortex[J].Journal of Chengdu University of Information Technology,2019,(04):172.[doi:10.16836/j.cnki.jcuit.2019.02.011]
[3]青 泉,罗 辉,陈刚毅.基于L波段秒级探空数据V-3θ图形的四川盆地暴雨预报模型研究[J].成都信息工程大学学报,2019,(02):186.[doi:10.16836/j.cnki.jcuit.2019.02.013]
QING Quan,LUO Hui,CHEN Gangyi.Forecasting Model of Torrential Rain in Sichuan Basin based on V-3θ
Structural Graphs of L-Band Second Level Sounding Data[J].Journal of Chengdu University of Information Technology,2019,(04):186.[doi:10.16836/j.cnki.jcuit.2019.02.013]
[4]吴秋月,华 维,申 辉,等.基于湿位涡与螺旋度的一次西南低涡强降水分析[J].成都信息工程大学学报,2019,(01):63.[doi:10.16836/j.cnki.jcuit.2019.01.013]
WU Qiuyue,HUA Wei,SHEN Hui,et al.Diagnostic Analysis of a Southwest Vortex Rainstormbased on Moist Potential Vorticity and Helicity[J].Journal of Chengdu University of Information Technology,2019,(04):63.[doi:10.16836/j.cnki.jcuit.2019.01.013]
[5]李潇濛,赵琳娜,肖天贵,等.2000-2015年青藏高原切变线统计特征分析[J].成都信息工程大学学报,2018,(01):91.[doi:10.16836/j.cnki.jcuit.2018.01.016]
LI Xiao-meng,ZHAO Lin-na,XIAO Tian-gui,et al.Statistical Characteristics Analysis of the Shear Linein the Qinghai-Tibet Plateau from 2000 to 2015[J].Journal of Chengdu University of Information Technology,2018,(04):91.[doi:10.16836/j.cnki.jcuit.2018.01.016]
[6]喻乙耽,马振峰,范广洲.华西秋雨气候特征分析[J].成都信息工程大学学报,2018,(02):164.[doi:10.16836/j.cnki.jcuit.2018.02.011]
YU Yi-dan,MA Zhen-feng,FAN Guang-zhou.The Analysis of Climatic Feature of Autumn Rainfall in West China[J].Journal of Chengdu University of Information Technology,2018,(04):164.[doi:10.16836/j.cnki.jcuit.2018.02.011]
[7]孙康慧,巩远发.20世纪70年代末云南省雨季降水的突变及原因分析[J].成都信息工程大学学报,2018,(02):177.[doi:10.16836/j.cnki.jcuit.2018.02.012]
SUN Kang-hui,GONG Yuan-fa.Abrupt Change of Precipitation in Rainy Season in YunnanProvince in Late 1970s and its Cause Analysis[J].Journal of Chengdu University of Information Technology,2018,(04):177.[doi:10.16836/j.cnki.jcuit.2018.02.012]
[8]吴树炎,顾建峰,刘海文,等.高原冬季雪深与重庆夏季降水的年际关系研究[J].成都信息工程大学学报,2018,(02):184.[doi:10.16836/j.cnki.jcuit.2018.02.013]
WU Shu-yan,GU Jian-feng,LIU Hai-wen,et al.Interannual Relationship between Winter Snow Depth over TibetanPlateau and Summer Precipitation over Chongqing[J].Journal of Chengdu University of Information Technology,2018,(04):184.[doi:10.16836/j.cnki.jcuit.2018.02.013]
[9]魏 凡,李 超.利用气象雷达信息划设雷暴飞行限制区的方法研究[J].成都信息工程大学学报,2018,(02):205.[doi:10.16836/j.cnki.jcuit.2018.02.016]
WEI Fan,LI Chao.Study on the Method of Setting Up Limited Flying area ofThunderstorm by Using Weather Radar Information[J].Journal of Chengdu University of Information Technology,2018,(04):205.[doi:10.16836/j.cnki.jcuit.2018.02.016]
[10]朱 莉,张腾飞,李华宏,等.云南一次短时强降水过程的中尺度特征及成因分析[J].成都信息工程大学学报,2018,(03):335.[doi:10.16836/j.cnki.jcuit.2018.03.017]
ZHU Li,ZHANG Teng-fei,LI Hua-hong,et al.Analysis on Meso-scale Features and Forming Reasons of a Short TimeIntensive Precipitation Case in Yunnan Province[J].Journal of Chengdu University of Information Technology,2018,(04):335.[doi:10.16836/j.cnki.jcuit.2018.03.017]
备注/Memo
Received date:2021-05-28
Foundation item:Project Supported by National Key R&D Program of China(2018YFC1507305); Special Project for the Development of Key Technologies for Weather Forecasting(YBGJXM20201A-06); Special Project for Forecasters of China Meteorological Administration(CMAYBY2020-026)