globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:5574845
论文题名:
海南台风暴雨的时空分布特征
其他题名: Spatial and temporal distribution characteristics of typhoon precipitation in Hainan
作者: 陆桂荣1; 王文1; 郑美琴2; 蔡亲波3
刊名: 大气科学学报
ISSN: 1674-7097
出版年: 2015
卷: 38, 期:5, 页码:710-715
语种: 中文
中文关键词: 台风暴雨 ; 时空分布 ; 气候特征 ; 海南
英文关键词: typhoon rainstorm ; spatial and temporal distributions ; climate characteristics ; Hainan
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 根据1966-2013年海南台风(热带气旋)个例资料和18个代表站的逐日降水资料,对影响海南的台风暴雨进行了统计分析。结果表明: 1)20世纪80年代以前为海南台风影响高峰期,以后为影响低发期。2)近48a海南台风暴雨的年均发生频次、降水量、降水量占全年总降水量的平均比例和最大比例都呈减少趋势,而台风过程最大降水量和日最大降水量则呈弱增加趋势。3)中路类登陆台风出现大暴雨以上降水的机率最大。4)EOF第一、第二特征向量场的空间分布分别为全区一致型、南北相反型。近48a海南台风暴雨降水呈现一种波动下降的趋势,具有准17 a、8a和3a的周期。
英文摘要: Based on the typhoon(tropical cyclone) cases influencing Hainan during 1966-2013 and the daily precipitation data of 18 stations, statistical analysis shows that: 1) The effect of Hainan typhoon is peak before 1980s,but it is opposite after 1980s. 2) The annual average occurrence frequency and precipitation of Hainan typhoon rainstorm during 1966-2013,and the average and maximum proportions of typhoon precipitation to annual total precipitation decrease,but the typhoon process maximum precipitation and daily maximum precipitation weakly increase. 3) The middle-path landing typhoon can make more heavy rainstorm. 4) The first and second eigenvector fields of EOF modes are the consistent positive or opposite pattern in all areas and the north-south opposite pattern, respectively. The precipitation of Hainan typhoon rainstorm shows a decreasing trend with fluctuation during 1966-2013,with quasi 17,8 and 3-yr periodic variations.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/156950
Appears in Collections:气候变化事实与影响

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作者单位: 1.南京信息工程大学大气科学学院, 南京, 江苏 210044, 中国
2.日照市气象局, 日照, 山东 276826, 中国
3.海南省气象台, 海口, 海南 570203, 中国

Recommended Citation:
陆桂荣,王文,郑美琴,等. 海南台风暴雨的时空分布特征[J]. 大气科学学报,2015-01-01,38(5):710-715
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