摘要
本文对8007号热带气旋与8221号热带气旋引起的北部湾增减水情况进行了计算,初步探讨了北部湾风暴潮特征与形成原因。研究表明,由于北部湾水深较浅,受地形影响,当热带气旋来临时,增减水现象较显著。广西外海受热带气旋外围影响时,水位呈现增减水振动,当距离热带气旋中心较近时,出现风暴潮。
In this paper,the water level fluctuation caused by tropical cyclones No. 8007 and No. 8221. in Beibu Gulf have been calculated. Based on the calculation, the characteristics and causes of storm surges in this sea area have been preliminarily analyzed. The results show that the phenomenon of water level fluctuation is re- markable due to landform when tropical cyclone comes. Being influenced by the outer area of tropical cyclone, the water level form fluctuation in the marginal seas adjacent to GuangXi. When the center of tropical cyclone approaches to this sea area, the water level fluctuation enhanced, and the storm surge emerged.
出处
《青岛远洋船员学院学报》
2006年第2期40-43,共4页
Journal of Qingdao Ocean Shipping Mariners College
关键词
北部湾
热带气旋
增减水
风暴潮
Beibu Gulf
Tropical cyclone
water level fluctuation
storm surge
