Wu Hongyu, Zou Yan, Liu Wei. Quantitative assessment of regional heavy rainfall process in Guangdong and its climatological characteristics. J Appl Meteor Sci, 2019, 30(2): 233-244. DOI: 10.11898/1001-7313.20190210.
Citation: Wu Hongyu, Zou Yan, Liu Wei. Quantitative assessment of regional heavy rainfall process in Guangdong and its climatological characteristics. J Appl Meteor Sci, 2019, 30(2): 233-244. DOI: 10.11898/1001-7313.20190210.

Quantitative Assessment of Regional Heavy Rainfall Process in Guangdong and Its Climatological Characteristics

More Information
  • Using daily precipitation data of 86 meteorological stations in Guangdong from 1961 to 2017, the standard of regional heavy rainfall process is defined. Assessment methods on composite intensity of regional heavy rainfall process in Guangdong are constructed, which take duration, range, maximum daily precipitation and maximum accumulated precipitation during the process into consideration. Characteristics and changes of the frequency, intensity and rain-waterlogging years of regional heavy rainfall process in Guangdong in recent 57 years are studied. 1211 regional heavy rainfall processes are captured, and the annual average frequency is 21.2 times. There are obvious interannual and interdecadal variations, the highest frequency occurs in 2016 (30 times), and the lowest occurs in 1963 (13 times). The annual frequency of regional heavy rainfall process in Guangdong increases at a rate of 0.08/(10 a) in recent 57 years, though not quite significant. The regional heavy rainfall process in Guangdong mainly occurs from April to September, accounting for 81.9% in the year, among which 45.4% processes occur in the first flood season (April-June), and 36.5% processes occur in the second flood season (July-September). The average duration of single regional heavy rainfall process in Guangdong is 2.3 d, and the longest is 17 d (9-25 June 1968). The average range of a single process covers 20.3 stations, and the process occurring on 28 January 2016 is observed by the most stations (83). The regional heavy rainfall process with the maximum composite intensity index occurs during 12-24 June 2005, reaching 1385.1 mm (Longmen), and this coincides "05.6" torrential rains and floods in Guangdong. The frequency and strength of the regional heavy rainfall process in Guangdong have intermonth, interannual and inter-decade variations, the frequency in May is the highest, and the strength in June is the highest. The annual harvest index of the rain waterlogging in Guangdong increases obviously at a rate of 0.17/(10 a) in recent 57 years. Regional heavy rainfall processes of relatively strong and strong class increase significantly, while those of relatively weak class decrease obviously in recent 57 years. Evaluation results show that there are five heavy rain waterlogging years, i.e., 2008, 2001, 1973, 1994, 1993.
  • Fig  1.   Variations of regional heavy rainfall frequency in Guangdong from 1961 to 2017

    Fig  2.   Ratio of mean regional heavy rainfall in Guangdong from 1961 to 2017

    Fig  3.   Variations of the harvest index of rain waterlogging in Guangdong from 1961 to 2017

    Fig  4.   Variations of regional heavy rainfall frequency with different class in Guangdong from 1961 to 2017

    (a)weak, (b)relatively weak, (c)medium, (d)relatively strong, (e)strong

    Fig  5.   Variations of the monthly mean strength index of regional heavy rainfall in Guangdong from 1961 to 2017

    Table  1   Correspondence between different percentile(P)and abnormal classes

    百分位数范围 暴雨过程异常等级
    0 < P < 60 1(弱)
    60≤P < 80 2(较弱)
    80≤P < 90 3(中等)
    90≤P < 95 4(较强)
    95≤P≤100 5(强)
    DownLoad: CSV

    Table  2   Correspondence between different percentile (P) and abnormal classes of rain-waterlogging years

    百分位数范围 年景等级
    0 < P≤10 1(弱)
    10 < P≤30 2(较弱)
    30 < P≤70 3(一般)
    70 < P≤90 4(较强)
    90 < P≤100 5(强)
    DownLoad: CSV

    Table  3   Regional heavy rainfall processes in Guangdong with composite intensity up to class Ⅴ (strong) from 1961 to 2017

    序号 暴雨发生时间 持续时间/d 范围/站 最大日降水量/mm 最大过程降水量/mm 综合强度指数
    1 2005-06-12—24 13 72 420.5 1385.1 29.9
    2 2001-06-02—13 12 63 605.3 1283.2 29.3
    3 1968-06-09—25 17 68 260.4 1069.3 25.9
    4 2003-06-06—16 11 58 566.3 911.2 24.8
    5 1994-07-18—28 11 58 560.4 888.6 24.5
    6 1994-06-08—20 13 72 523.5 691.2 24.4
    7 1977-05-25—06-01 8 44 621.6 1196.5 23.7
    8 1975-05-10—22 13 63 300.4 1012.2 22.8
    9 1993-06-03—18 16 72 199.1 774.3 22.2
    10 1998-06-19—26 8 56 398 1183.9 20.9
    11 2017-06-13—22 10 59 362.7 944.9 20.8
    12 1987-05-20—22 3 49 620.1 1024.1 20.2
    13 1992-06-07—15 9 66 312 871.3 19.5
    14 2008-05-29—6-7 10 59 346.9 757.9 19.1
    15 1997-07-01—11 11 54 277.6 839.3 18.6
    16 1973-05-06—13 8 65 324.2 801.2 18.5
    17 2001-08-27—09-05 10 70 286.8 684.5 18.4
    18 1998-05-29—06-06 9 42 433.1 761.5 17.9
    19 2008-06-10—18 9 72 376.5 611.8 17.5
    20 1982-05-10—13 4 23 640.6 823.5 17.2
    21 1965-09-27—10-01 5 36 433.1 927.7 16.6
    22 2014-05-15—23 9 41 288.7 924.7 16.5
    23 1979-09-23—25 3 40 547.3 809.5 16.3
    DownLoad: CSV

    Table  4   lnterannual variations of the harvest pattern index of rain-waterlogging and direct economic loss in Guangdong from 1994 to 2017

    年份 雨涝年景指数 评估等级 直接经济损失/亿元
    1994 2.11 5 170.00
    1995 0.53 4 10.83
    1996 -0.46 3 4.86
    1997 0.86 4 37.10
    1998 1.21 4 54.11
    1999 -1.13 2 0.00
    2000 0.45 3 5.61
    2001 2.25 5 11.47
    2002 0.34 3 16.11
    2003 0.2 3 6.42
    2004 -1.27 1 2.96
    2005 0.74 4 56.32
    2006 1.28 4 21.00
    2007 -0.63 3 19.75
    2008 2.81 5 83.81
    2009 -0.44 3 8.22
    2010 1.02 4 54.81
    2011 -0.88 2 10.55
    2012 -0.98 2 29.16
    2013 0.34 3 189.65
    2014 -0.1 3 79.52
    2015 0.29 3 16.07
    2016 0.57 4 27.36
    2017 -0.06 3 21.60
    DownLoad: CSV

    Table  5   Frequency and ratio of different level of regional heavy rainfall processes in Guangdong from 1961 to 2017

    年份 1级 2级 3级 4级 5级 平均强度指数
    次数 比率/% 次数 比率/% 次数 比率/% 次数 比率/% 次数 比率/%
    1961—1970年 121 61.1 45 22.7 19 9.6 11 5.6 2 1.0 2.7
    1971—1980年 128 57.6 49 22.1 24 10.8 17 7.7 4 1.8 3.0
    1981—1990年 150 65.8 43 18.9 15 6.5 18 7.9 2 0.9 2.7
    1991—2000年 119 57.8 42 20.4 22 10.7 16 7.7 7 3.4 3.3
    2001—2010年 113 57.4 37 15.7 25 12.7 22 11.2 6 3.0 3.7
    2011—2017年 104 65.0 25 15.6 14 8.8 15 9.4 2 1.2 2.9
    DownLoad: CSV
  • 何立富, 陈涛, 孔期.华南暖区暴雨研究进展.应用气象学报, 2016, 27(5):559-569. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20160505&flag=1
    赵玉春, 王叶红.近30年华南前汛期暴雨研究概述.暴雨灾害, 2009, 28(3):193-202;228. DOI: 10.3969/j.issn.1004-9045.2009.03.001
    谢炯光, 纪忠萍, 谷德军, 等.广东省前汛期连续暴雨的气候背景及中期环流特征.应用气象学报, 2002, 24(2):17-19. http://d.old.wanfangdata.com.cn/Periodical/yyqxxb200603013
    彭丽英, 王谦谦, 马慧.华南前汛期暴雨气候特征的研究.南京气象学院学报, 2006, 29(2):249-253. DOI: 10.3969/j.issn.1674-7097.2006.02.016
    郑彬, 梁建茵, 林爱兰, 等.华南前汛期的锋面降水和夏季风降水1.划分日期的确定.大气科学, 2006, 50(6):1207-1216. DOI: 10.3878/j.issn.1006-9895.2006.06.15
    张婷, 魏凤英.华南地区汛期极端降水的概率分布特征.气象学报, 2009, 67(3):442-451. DOI: 10.3321/j.issn:0577-6619.2009.03.011
    王东海, 夏茹娣, 刘英.2008年华南前汛期致洪暴雨特征及其对比分析.气象学报, 2011, 69(1):137-148. http://d.old.wanfangdata.com.cn/Periodical/qxxb201101012
    伍红雨, 杜尧东, 秦鹏.华南暴雨的气候特征及变化.气象, 2011, 37(10):1262-1269. DOI: 10.7519/j.issn.1000-0526.2011.10.009
    伍红雨, 杜尧东, 陈桢华, 等.华南雨日、雨强的气候变化.热带气象学报, 2011, 27(6):877-888. DOI: 10.3969/j.issn.1004-4965.2011.06.011
    张端禹, 徐明, 汪小康, 等.华南前汛期持续暴雨环流特征分析.暴雨灾害, 2012, 31(3):264-271. http://d.old.wanfangdata.com.cn/Periodical/hbqx201203010
    林爱兰, 李春晖, 郑彬, 等.广东前汛期持续性暴雨的变化特征及其环流形势.气象学报, 2013, 71(4):628-642. http://d.old.wanfangdata.com.cn/Periodical/qxxb201304004
    林爱兰, 谷德军, 郑彬, 等.6月广东持续性暴雨过程概念模型的建立.热带气象学报, 2015, 31(3):289-299. http://d.old.wanfangdata.com.cn/Periodical/rdqxxb201503001
    林爱兰, 谷德军, 李春晖, 等.广东6月持续性暴雨期间的大气环流异常.气象学报, 2015, 73(5):803-818. http://d.old.wanfangdata.com.cn/Periodical/qxxb201505001
    卞洁, 李双林, 何金海.长江中下游地区洪涝灾害风险性评估.应用气象学报, 2011, 22(5):604-611. DOI: 10.3969/j.issn.1001-7313.2011.05.011
    郑国, 薛建军, 范广洲, 等.淮河上游暴雨事件评估模型.应用气象学报, 2011, 22(6):753-759. DOI: 10.3969/j.issn.1001-7313.2011.06.014
    扈海波, 轩春恰, 诸立尚.北京地区城市暴雨积涝灾害风险预评估.应用气象学报, 2013, 24(1):99-108. DOI: 10.3969/j.issn.1001-7313.2013.01.010
    甘衍军, 徐晶, 赵平, 等.暴雨致洪预报系统及其评估.应用气象学报, 2017, 28(4):385-398. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20170401&flag=1
    李春梅, 刘锦銮, 潘蔚娟, 等.暴雨综合影响指标及其在灾情评估中的应用.广东气象, 2008, 30(4):1-4. DOI: 10.3969/j.issn.1007-6190.2008.04.001
    罗艳艳, 何金海, 邹燕, 等.华南前汛期雨涝强、弱年的确定及其环流特征对比.气象科学, 2015, 35(2):160-166. http://d.old.wanfangdata.com.cn/Periodical/qxkx201502006
    邹燕, 叶殿秀, 林毅, 等.福建区域性暴雨过程综合强度定量化评估方法.应用气象学报, 2014, 25(3):360-364. DOI: 10.3969/j.issn.1001-7313.2014.03.014
    Hyndman R J, Fan Y N.Sample quantiles in statistical packages.Am Statist, 1996, 50(4):361-365. DOI: 10.1080/00031305.1996.10473566
    广东省防灾减灾年鉴编写组.广东省防灾减灾年鉴(1994-2016年卷).广州: 岭南美术出版社, 1995-2017.
    宋丽莉.中国气象灾害大典(广东卷).北京:气象出版社, 2006.
    广东省地方史志编纂委员会编.广东省志(自然灾害志).广州: 广东人民出版社, 2001.
    叶萌, 张东, 何夏江."05.6"广东致洪暴雨过程的预报着眼点.广东气象, 2006, 28(1):35-38. DOI: 10.3969/j.issn.1007-6190.2006.01.010
    何立富, 周庆亮, 陈涛."05.6"华南暴雨中低纬度系统活动及相互作用.应用气象学报, 2010, 21(4):387-394. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20100401&flag=1
    张德苏, 刘作挺, 梁国锋, 等.阳江市2001年6月7到8日连续特大暴雨过程分析.广东气象, 2002, 24(2):17-19. DOI: 10.3969/j.issn.1007-6190.2002.02.006
    李丽平, 章开美, 王超, 等.近40年华南前汛期极端降水时空演变特征.气候与环境研究, 2010, 15(4):443-450. DOI: 10.3878/j.issn.1006-9585.2010.04.12
    李丽平, 许冠宇, 成丽萍, 等.华南后汛期极端降水特征及变化趋势.南京气象学院学报, 2012, 35(5):570-577. DOI: 10.3969/j.issn.1674-7097.2012.05.007
    徐雨晴, 苗秋菊, 沈永平.2008年:气候持续变暖, 极端事件频发.气候变化研究进展, 2009, 5(1):56-60. DOI: 10.3969/j.issn.1673-1719.2009.01.011
    张培群, 贾小龙, 王永光.2008年海洋和大气环流异常及对中国气候的影响.气象, 2009, 35(4):112-116. http://d.old.wanfangdata.com.cn/Periodical/qx200904015
    王婷, 胡娅敏, 潘蔚娟.2008年广东"史上最强龙舟水"的气候成因.广东气象, 2008, 30(4):5-7. DOI: 10.3969/j.issn.1007-6190.2008.04.002
    薛纪善.1994年华南夏季特大暴雨研究.北京:气象出版社, 1999.
    陈超, 卢山, 任志杰, 等.强西南季风背景下1311号台风"尤特"的暴雨特征分析.广东气象, 2015, 37(2):13-17. DOI: 10.3969/j.issn.1007-6190.2015.02.003
    林建, 杨贵名.近30年中国暴雨时空特征分析.气象, 2014, 40(7):816-856. http://d.old.wanfangdata.com.cn/Periodical/qx201407005
  • Related Articles

    [1]Zou Yan, Ye Dianxiu, Lin Yi, Liu Aiming. A Quantitative Method for Assessment of Regional Heavy Rainfall Intensity[J]. Journal of Applied Meteorological Science, 2014, 25(3): 360-364.
    [2]Gong Zhiqiang, Wang Xiaojuan, Cui Donglin, Wang Yanjiao, Ren Fumin, Feng Guolin, Zhang Qiang, Zou Xukai, Wang Xiaoling. The Identification and Changing Characteristics of Regional Low Temperature Extreme Events[J]. Journal of Applied Meteorological Science, 2012, 23(2): 195-204.
    [3]Xie Jiongguang, Ji Zhongping, Gu Dejun, Li Xiaojuan, Hu Litian. Climate Characteristics and Cause of Long Continuous Rainstorm Process in June of Guangdong Province[J]. Journal of Applied Meteorological Science, 2012, 23(2): 174-183.
    [4]Feng Jianshe, Wang Jianyuan, Wang Xintang, Xue Xiaoping, Chen Yanchun, Li Hongyi, Fan Liju. The Application of Relative Humidity Index to Agricultural Drought Monitoring[J]. Journal of Applied Meteorological Science, 2011, 22(6): 766-772.
    [5]Zhao Haiyan, Gao Ge, Zhang Peiqun, Yan Xiaodong. The Modification of Meteorological Drought Composite Index and Its Application in Southwest China[J]. Journal of Applied Meteorological Science, 2011, 22(6): 698-705.
    [6]Li Xia, Liang Jianyin, Zheng Bin. Interdecadal Variabilities of SCS Summer Monsoon Intensity[J]. Journal of Applied Meteorological Science, 2007, 18(3): 330-339.
    [7]Hong Mei, Zhang Ren, Wu Guoxiong, He Jinhai, Yu Dandan. Fuzzy Clustering Diagnosing and Forecasting on Subtropical High Intensity Index[J]. Journal of Applied Meteorological Science, 2006, 17(4): 459-466.
    [8]He Min. Relationship Between Tropical Circulation Intensity and Summer Precipitation Anomaly in China[J]. Journal of Applied Meteorological Science, 1999, 10(2): 171-180.
    [9]Synthetical Indexes of the Disaster of Snow Cover[J]. Journal of Applied Meteorological Science, 1998, 9(1): 119-123.
    [10]Lin Mingzhi Li Xufang Yu Heshu, . A Compositive Criterion for Forecasting Explosive Cyclogenesis in the Western North Pacific[J]. Journal of Applied Meteorological Science, 1993, 4(1): 112-116.
  • Cited by

    Periodical cited type(44)

    1. 陈训来,徐婷,王蕊,李媛,张舒婷,王书欣,王明洁,陈元昭. 珠江三角洲“9·7”极端暴雨精细观测特征及成因. 应用气象学报. 2024(01): 1-16 . 本站查看
    2. 伍红雨,郭尧,吴遥. 近62 a华南“龙舟水”气候特征及变化. 暴雨灾害. 2024(01): 84-92 .
    3. 王荣,叶殿秀,肖潺,赵珊珊,陈鲜艳,李威. 近62 a三峡地区区域性暴雨过程气候特征及长期变化规律. 水利水电技术(中英文). 2024(02): 16-26 .
    4. 杜青平,程浩,高伟,陈岩,张远. 2014—2019年东江干流氮磷通量传输特征与源解析. 环境科学学报. 2024(03): 139-149 .
    5. 伍红雨,吴遥,郑璟. 2022年华南极端“龙舟水”与大气环流及海温异常的关系. 大气科学学报. 2024(03): 450-459 .
    6. 郑璟,陈卓煌,李文媛,唐力生. 广东省台风巨灾指数保险的研发与应用. 热带地理. 2024(06): 1139-1148 .
    7. 郑璟,刘蔚琴,李文媛,庄燕洵. 2022年广东省气候特征及其影响. 广东气象. 2024(03): 9-13 .
    8. 苗蕾,王志,李蔼恂,冯蕾. 2022年“龙舟水”期间华南地区降水对公路交通的影响. 气象与减灾研究. 2024(01): 65-71 .
    9. 赵亮,魏铁鑫,王丽荣,张安凝知. 基于综合强度指数和受灾面积的区域性暴雨过程的客观识别及特征分析. 气候与环境研究. 2024(04): 430-442 .
    10. 高铭祥,梁之彦,张兰,张锦城,郝笑,廖菲. 广州市区暴雨预警信号发布策略优化研究. 广东气象. 2024(06): 69-72 .
    11. 李倩,林益同,周晓宇,房一禾. 1961—2021年辽宁省区域性暴雨过程综合强度时空变化分析. 气象与环境学报. 2024(06): 53-61 .
    12. 赵亮,魏铁鑫,王丽荣,解文娟. 基于多维特征的区域性暴雨过程相似性检索方法研究. 热带气象学报. 2024(06): 966-973 .
    13. 余锐,孙丽颖,张菁,陈晓旸,陶然. 广东大范围持续干旱过程的识别及其环流成因分析. 中国农村水利水电. 2023(03): 21-29+38 .
    14. 伍红雨,邹燕,郭尧. 损失率评估模型在广东气象灾害损失评估中的应用. 气象. 2023(06): 757-764 .
    15. 王振超,陈雪娇,刘姝,花家嘉,刘文忠. 微型智能气象站降雨观测对比试验. 应用气象学报. 2023(04): 438-450 . 本站查看
    16. 王芬,洪国平,赵小芳,何明琼,刘静,罗金芳,邓凯. 暴雨过程致灾危险性评估方法研究——以孝感市“8·12”暴雨过程为例. 暴雨灾害. 2023(06): 724-730 .
    17. 李娴茹,韦志刚,刘雨佳,王欢,马力,郭仕侗. 1961~2018年华南全年和四季暴雨的时空特征分析. 气候与环境研究. 2022(01): 1-18 .
    18. 伍红雨,吴遥,郭尧. 华南冬季区域性暴雨过程强度异常的成因分析. 中山大学学报(自然科学版)(中英文). 2022(02): 8-17 .
    19. 黎跃勇,周威,李好,梁可. 基于优势分析法的暴雨综合致灾指数及阈值研究——以张家界市保险业为例. 暴雨灾害. 2022(02): 232-239 .
    20. 伍红雨,李文媛,段海来,郑璟. 2021年广东省气候概况. 广东气象. 2022(02): 1-5 .
    21. 何际斌. 潖江“2020.6”特大暴雨洪水分析. 水利科学与寒区工程. 2022(04): 63-65 .
    22. 李莹,王国复. 气象灾害风险管理系统设计与应用. 应用气象学报. 2022(05): 628-640 . 本站查看
    23. 解明恩,陈鲜艳,张文千,邹旭恺,张存杰. 雨涝指数在云南洪涝灾害监测中的应用. 灾害学. 2022(03): 77-83 .
    24. Yueyong LI,Wei ZHOU,Hao LI,Ke LIANG. Study on Torrential Rain Disaster Index and Threshold in Zhangjiajie City. Meteorological and Environmental Research. 2022(05): 60-67+72 .
    25. 吴东少,高伟,陈岩,张远. 基于改进LAM模型的河流污染源解析方法与例证. 环境科学学报. 2022(12): 376-383 .
    26. 许丹,张东海. 贵州区域性暴雨过程的定量化评估及气候特征. 中低纬山地气象. 2022(06): 1-8 .
    27. 王娟怀,李清泉,汪方,杨守懋,胡娅敏. 基于DERF2.0的华南前汛期降水订正. 应用气象学报. 2021(01): 115-128 . 本站查看
    28. 张柳红,郑璟,伍红雨,刘东玲. 广东暴雨洪涝灾害损失定量评估. 暴雨灾害. 2021(01): 87-93 .
    29. 王莉萍,王铸,连治华,刘璐. 基于小时分辨率的降水过程辨识方法研究. 暴雨灾害. 2021(01): 12-18 .
    30. 伍红雨,郭尧,邹燕,陈卓煌. 华南区域性暴雨过程的客观评估及异常机理分析. 暴雨灾害. 2021(03): 306-315 .
    31. 周杰,赵俊虎,李永华,邹旭恺. 西南地区东部区域性暴雨事件的客观识别及其变化特征. 高原气象. 2021(04): 789-800 .
    32. 张正秋,祝从文,苏京志,刘伯奇,蒋宁,陈昊明. 气候动力诊断和分析系统设计与应用. 应用气象学报. 2021(05): 542-552 . 本站查看
    33. 陆芊芊,黄卓. 广西台风与非台风暴雨时空变化特征差异分析. 气象研究与应用. 2021(03): 12-17 .
    34. 林佩贤,田刚,李超. 湖北省区域性暴雨雨团识别及特征分析. 暴雨灾害. 2021(05): 505-512 .
    35. 罗聪,时洋,吴乃庚,张华龙,黄晓莹,苏冉. 基于邻域最优概率的GRAPES快速更新循环同化预报系统逐时降水订正方法. 热带气象学报. 2021(04): 569-578 .
    36. 陈鲜艳,李威,张强,邹旭恺,吴秋洁. 长江中下游地区雨涝指数构建及其应用. 水科学进展. 2021(06): 834-842 .
    37. 梁振清,陈生. 基于深度学习和雷达观测的华南短临预报精度评估. 气象研究与应用. 2020(01): 41-47 .
    38. 陈芳丽,李明华,姜帅,黄潮,曾丹丹,陈颖. 粤北暴雨中心的降水气候特征分析. 广东气象. 2020(01): 10-14 .
    39. 魏玥玥. 贵溪2017年三次大暴雨过程分析. 农家参谋. 2020(05): 126+157 .
    40. 董晓云,余锦华,梁信忠,王琛. CWRF模式极端降水模拟误差订正. 应用气象学报. 2020(04): 504-512 . 本站查看
    41. 林爱兰,谷德军,彭冬冬,郑彬,李春晖. 体现大尺度特征的区域持续性强降水过程定义指标. 热带气象学报. 2020(03): 289-298 .
    42. 洪国平. 区域性暴雨过程评价指标在湖北的本地化修订与应用. 暴雨灾害. 2020(05): 470-476 .
    43. 周幼婵,何林宴,林雪香,杨晴. 广西贵港市暴雨过程综合强度评估及分析. 气象研究与应用. 2020(03): 27-31 .
    44. 伍红雨,邹燕,郭尧. 广东气候年景的客观定量化评估. 大气科学学报. 2020(03): 516-524 .

    Other cited types(3)

Catalog

    Figures(5)  /  Tables(5)

    Article views3522 PDF downloads245 Cited by: 47
    • Received : 2018-08-01
    • Accepted : 2019-01-15
    • Published : 2019-03-30

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return