摘要
依据小洋山1997年8月至2002年12月的实测潮位,采用王骥、方国洪的分潮模式,进行潮汐调和分析,给出天文潮预报,对期间的实测潮位进行增、减水分离,获取洋山深水港区风暴增、减水特征,以及典型的风暴的增减水过程,经对1998—2002年实测资料分离,≥30cm的增水年均17.2场,≥30cm的减水年均9场,引发严重增水的主要是台风。同时检索、比对大量的台风资料,分析引发洋山港海域严重和特大风暴潮的台风路径主要是在浙江北部到长江口沿海登陆的台风和在浙江北部、上海市近海北上或转向的台风。
Based on the measured tide level data between Aug, in 1997 and Dec, 2000, harmonic analysis was taken on with the method of tidal component mode created Wangji and Fangguohong. The astronomic tide was made and the typical process and characteristics of storm surges at the Yangshan port were obtained. Aider analyzing a great deal of typhoon data, the paper got the main typhoon tracks which caused serious storm surges at the Yangshan port.
出处
《海洋通报》
CAS
CSCD
北大核心
2008年第3期19-24,共6页
Marine Science Bulletin
