南麂海域台风波浪的波型分析  

ANALYSIS OF WAVE PATTERN IN HURRICANE WAVE IN NANJI SEA AREA

作　　者：黄树生[1] 

机构地区：[1]国家海洋局第二海洋研究所,杭州310012

出　　处：《海洋通报》1995年第6期19-23,共5页Marine Science Bulletin

摘　　要：以南麂海洋站1983～1989年实测台风波浪资料为依据,分析了台风影响过程中测点波型的演变,对台风浪的波陡与波型、风速与波型之间的关系进行讨论.从而得出,台风影响过程中本区出现较大波浪的波型绝大部分属于风浪,6级以上风速作用时,本区台风浪均属于风浪波型,从而可以断定,不同重现期的台风波浪应属于风浪.Based on observational data of hurricane wave at Nanji oceanographic station between 1983-1989, the evolvements of observational wave pattern in hurricane wave are analysed. The relationships between wave slope and wave pattern and that between wind speed and wave pattern are discussed. The results show that wave pattern of larger wave in the region is largely that of wind wave and , when wind speed over Beaufort force six, totally that of wind wave. It can be concluded that the hurricane wave of different reappearance is wind wave.

关 键 词：南麂海域 台风 波浪 波型 

分 类 号：P731.22[天文地球—海洋科学]