[1]陈冰,陆卫华,宋祖钦,等.茂名地区极端降水时空分布特征分析[J].气象研究与应用,2018,39(01):6-10.
 Chen Bing,Lu Wei-hua,Song Zu-qin,et al.Temporal and Spatial Distributions of Extreme Precipitation in Maoming Area[J].Journal of Meteorological Research and Application,2018,39(01):6-10.
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茂名地区极端降水时空分布特征分析()
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气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第39卷
期数:
2018年01期
页码:
6-10
栏目:
天气气候
出版日期:
2018-03-31

文章信息/Info

Title:
Temporal and Spatial Distributions of Extreme Precipitation in Maoming Area
作者:
陈冰1 陆卫华2 宋祖钦1 陈蔚烨1 李英1
1. 广东省化州市气象局, 广东化州, 525100;
2. 广东省高州市气象局, 广东高州, 525200
Author(s):
Chen Bing1 Lu Wei-hua2 Song Zu-qin1 Chen Wei-ye1 Li Ying1
1. Meteorological Bureau of Huazhou City, Guangdong Prouinoe, Huazhou Guangdong 525100;
2. Meteorological Bureau of Gaozhou City, Guangdong Prouinoe, Gaozhou Guangdong 525200
关键词:
茂名地区极端降水极端降水指数变化特征
Keywords:
Maoming areaextreme precipitationextreme precipitation indexvariation characteristics
分类号:
P46
摘要:
利用茂名地区近45a气象站逐日雨量资料,分析茂名极端降水事件的时空分布特征。结果表明,茂名地区各站极端降水的阈值与强度由南向北递减,平均年极端降水总量由西向东递减,极端降水频次的由西北向东南递减;极端降水事件发生的高峰月为6月,极端降水总量峰值月为8月;茂名地区极端降水总量、频数以及强度均呈增加趋势,年际变化明显;各极端降水指标突变特征不明显;年极端降水总量以及频次存在准3a短周期、12a长周期。
Abstract:
Based on the daily rainfall data of 45 meteorological stations in Maoming area, this paper analyzed the temporal and spatial distribution characteristics of the extreme precipitation events in Maoming. The analysis showed that the threshold and intensity of extreme precipitation decreased from south to north, the average annual total precipitation decreased from west to east, and the frequency of extreme precipitation decreased from northwest to southeast. The occurrence of extreme precipitation events peaked in June and the total precipitation peaked in August. The total precipitation, frequency, and intensity of extreme precipitation in Maoming area tended to increase, and the inter-annual variation was distinct. The characteristics of sudden change of extreme precipitation index were not obvious. The annual total precipitation and frequency exist quasi-3a short cycle, 12a long cycle.

参考文献/References:

[1] 广东省气候变化评估报告编制课题组.广东气候变化评估报告(节选)[J].广东气象,2007,29(3):1-2.
[2] http://www.docin.com/p-783487595.html
[3] 林良勋,冯业荣,黄忠,等.广东省天气预报技术手册[M].北京:气象出版社,2006:86-93.
[4] 吴慧,邹燕,朱晶晶,等.海南省区域性暴雨过程综合强度评估方法研究[J],气象研究与应用,2017,38(3):8-12.
[5] 程正泉,项颂翔,黄晓莹,等."凡亚比"登陆引发粤西大范围强降水的对流降水分析[J].广东气象,2013,35(1):14-18.
[6] 钟雄蔼,杨廷春,彭可泉,等."5.20信宜市特大暴雨过程诊断分析[J],广东气象,2016,38(6):28-30.
[7] 钱维宏,符娇兰,张玮玮,等.近40年中国平均气候与极值气候变化的概述[J].地球科学进展,2007,22(7):673-684.
[8] 秦大河,丁一汇,苏纪兰,等.中国气候与环境演变评估(I):中国气候与环境变化及未来趋势[J].气候变化研究进展,2006,1(1):4-9.
[9] 肖伟军,陈炳洪,刘云香.近45a华南夏季降水时空演变特征[J].气象研究与应用,2009,30(1):12-14,22.
[10] 覃卫坚,李耀先,覃志年.广西暴雨的区域性和连续性研究[J].气象研究与应用,2012,33(4):1-4.
[11] 周绍毅,苏志,李强.广西5个主要极端降水指数变化趋势分析[J].气象研究与应用,2012,33(3):8-13.
[12] 黄明策.广西暴雨时空分布特征[J].广西气象,2006,27(3):34-36,50.
[13] 丘平珠,唐炳莉.广西降雨强度的气候分析[J].气象研究与应用,2007,38(3):45-48.
[14] 黄雪松,周惠文,黄梅丽,等.广西近50年来气温、降水气候变化[J].广西气象,2005,26(4):9-11.
[15] 王艺,蓝求,李雯雯.柳州市短历时暴雨变化特征分析[J].气象研究与应用,2016,37(3):84-86,97.
[16] 周绍毅,卢小凤,罗红磊.南宁市短历史暴雨演变特征分析[J].气象研究与应用,2016,37(1):64-67.
[17] 陈冰,江满桃,郭潮升,等.化州暴雨气候特征分析及极端事件重现期计算[J].气象研究与应用,2014,35(4):19-23.
[18] IPCC.Climate change 2013:thephysical science basic[R].Cambridge:Cambridge University Press,2013.
[19] 翟盘茂,潘晓华.中国北方近50年温度和降水极端事件变化[J].地理学报,2003,58(9):1-10.
[20] RAOK,PATWARDHAN S,KULKARNIA,etal.Projected change in mean and extreme precipitation indices over India using PRECIS[J].Global & Planetary Change,2014,113(2):77-90.
[21] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,2009:27-29.
[22] Xu Z X, Takeuchi K, Ishidaira H. Monotonic trend and step changes in Japaneseprecipitation[J].Journalof Hydrology, 2003,279(1-4):144-150.
[23] 王芬,孙旭东,杨溢.黔西南暴雨多时间尺度特征及其天气学成因分析[J].气象研究与应用,2015,36(2):15-20.
[24] 林振山,邓自旺.子波气候诊断技术的研究[M].北京:气象出版社,1999:1-36.
[25] 陆虹,陈思蓉,郭媛,等.近50年华南地区极端强降水频次的时空变化特征[J].热带气象学报,2012,28(2):219-227.
[26] 伍红雨.华南暴雨的气候特征及变化[J].气象,2011,37(10):1262-1269.

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备注/Memo

备注/Memo:
收稿日期:2017-12-19。
基金项目:茂名市气象局课题"茂名极端降水天气天气触发机制及预报预警技术研究"。
作者简介:陈冰(1973-),女,高级工程师,主要从事天气预测及气象服务工作。E-mail:522033051@qq.com。
更新日期/Last Update: 1900-01-01