CAJ | 학술논문

选取2004～2014年登陆和影响海陵湾附近海域四种典型路径的代表台风作为研究对象，运用 SWAN41.01版本，通过大区粗网格、小区细网格两重嵌套的方法对台风影响过程所产生的台风浪进行较高分辨率的模拟研究，结合海陵湾不同位置的地形特征及台风中心与海陵湾的相对位置分析台风浪分布特征．分别利用附近海域大万山、闸坡和硇洲海洋站海浪观测值与模拟结果进行检验．模拟结果表明：模式计算结果与实测结果吻合性较好．台风中心位于海陵湾邻近海域的不同位置，台风强度及生命历程的不同，所引起的台风浪有效波高极值及持续时间都有着较大的差异，而不同的路径的台风引起的台风浪场分布也呈现出明显不同的特征．本研究可以为整个海陵湾邻近海域台风浪分布特征的了解与认识提供较好的参考．
선취2004～2014년등륙화영향해릉만부근해역사충전형로경적대표태풍작위연구대상，운용 SWAN41.01판본，통과대구조망격、소구세망격량중감투적방법대태풍영향과정소산생적태풍랑진행교고분변솔적모의연구，결합해릉만불동위치적지형특정급태풍중심여해릉만적상대위치분석태풍랑분포특정．분별이용부근해역대만산、갑파화뇨주해양참해랑관측치여모의결과진행검험．모의결과표명：모식계산결과여실측결과문합성교호．태풍중심위우해릉만린근해역적불동위치，태풍강도급생명역정적불동，소인기적태풍랑유효파고겁치급지속시간도유착교대적차이，이불동적로경적태풍인기적태풍랑장분포야정현출명현불동적특정．본연구가이위정개해릉만린근해역태풍랑분포특정적료해여인식제공교호적삼고．
Typhoons of 4 typical path landing or affecting Hailing Bay during 2004 ~2014 are selected in this study. The typhoon wave is simulated by the method of double nested of SWAN 41.01,combined the large coarse grid with small fine grid.The distribution of typhoon wave field is studied based on the paths of typhoon,the topograph-ic features at different positions and the position of typhoon center relative to the bay.Used observed data from Dawanshan,Zhapo and Naozhou stations the simulation result is tested.It shows that the simulation results is proved well by comparison with the observed data.The differences of the wave field inside and outside Hailing Bay is significant.The peak value and duration of significant wave height is different when typhoon center is located at different position near Hailing Bay or the intensity or life course is different.And the typhoon wave field distribution caused by different path is also different.The simulation can provide a good reference to understand the distribution of typhoon wave field near Hailing Bay.