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青岛沿海风暴潮分析
引用本文:张晓慧,盛春雁,邵滋和.青岛沿海风暴潮分析[J].海洋预报,2006,23(Z1):42-46.
作者姓名:张晓慧  盛春雁  邵滋和
作者单位:北海舰队海洋水文气象中心,青岛,266003
摘    要:利用“青岛海军验潮站”(青岛大港1号码头)1949~2003年潮汐资料,采用统计风暴高潮位≥510cm出现频数的方法,对青岛沿海风暴潮进行统计分析。结果表明:诱发青岛沿海显著风暴高潮位的天气系统都是台风,集中出现在8月下旬~9月上旬,阴历初三至初五、十五至十八两个天文大潮时段。

关 键 词:青岛  风暴高潮位  诱因分析
文章编号:1003-0239(2006)增刊-0042-05
修稿时间:2005年1月31日

Analysis of storm surge at coastal area of Qingdao
ZHANG Xiao-hui,SHENG Chun-yan,SHAO Zi-he.Analysis of storm surge at coastal area of Qingdao[J].Marine Forecasts,2006,23(Z1):42-46.
Authors:ZHANG Xiao-hui  SHENG Chun-yan  SHAO Zi-he
Abstract:The tide data (1949~2003) from naval tide station of Qingdao are used to analyzestorm surge at coastal area of Qingdao by statistical method. The frequence of tide levelgreater than or equal to 510cm is counted. The auther found that the weather systemsinducing storm surge are all typhoon which mostly appear between the last ten days ofAugust and the first ten days of September. The time by lunar calendar is from the thirdto fifth day of a month and from the fifteenth to eighteenth day of a month, which is theastronomical spring tide period.
Keywords:Qingdao  Storm surge  inducement analysis
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