海洋通报
海洋通報
해양통보
Marine Science Bulletin
2015年
5期
592-599
,共8页
江苏沿海%台风达维%台风浪%有效波高
江囌沿海%檯風達維%檯風浪%有效波高
강소연해%태풍체유%태풍랑%유효파고
the sea off Jiangsu coast%typhoon DAMREY%typhoon waves%significant wave height
2012年10号台风"达维"是历史上登陆长江以北的最强台风.以NCEP风场和Jelesnianski经验模型构造台风风场,利用波浪谱模型SWAN对"达维"影响期间江苏海域台风浪进行数值模拟,模拟结果和实测结果吻合较好.在利用实测风、波浪资料验证的基础上分析江苏海域台风浪的时空分布特征."达维"影响期间,测风塔100 m高度实测最大风速为42.2 m/s,实测最大波高为6.17 m.数值模式结果显示江苏外海有效波高最大值超过9 m,台风移向的中心右侧风速和有效波高均较大,波向基本与风向一致;在台风移向的中心左侧一般风速较小,风速和有效波高也均比右侧小,波向与风向不一致.在近岸台风浪要素受地形影响较大,与外海特点不同.
2012年10號檯風"達維"是歷史上登陸長江以北的最彊檯風.以NCEP風場和Jelesnianski經驗模型構造檯風風場,利用波浪譜模型SWAN對"達維"影響期間江囌海域檯風浪進行數值模擬,模擬結果和實測結果吻閤較好.在利用實測風、波浪資料驗證的基礎上分析江囌海域檯風浪的時空分佈特徵."達維"影響期間,測風塔100 m高度實測最大風速為42.2 m/s,實測最大波高為6.17 m.數值模式結果顯示江囌外海有效波高最大值超過9 m,檯風移嚮的中心右側風速和有效波高均較大,波嚮基本與風嚮一緻;在檯風移嚮的中心左側一般風速較小,風速和有效波高也均比右側小,波嚮與風嚮不一緻.在近岸檯風浪要素受地形影響較大,與外海特點不同.
2012년10호태풍"체유"시역사상등륙장강이북적최강태풍.이NCEP풍장화Jelesnianski경험모형구조태풍풍장,이용파랑보모형SWAN대"체유"영향기간강소해역태풍랑진행수치모의,모의결과화실측결과문합교호.재이용실측풍、파랑자료험증적기출상분석강소해역태풍랑적시공분포특정."체유"영향기간,측풍탑100 m고도실측최대풍속위42.2 m/s,실측최대파고위6.17 m.수치모식결과현시강소외해유효파고최대치초과9 m,태풍이향적중심우측풍속화유효파고균교대,파향기본여풍향일치;재태풍이향적중심좌측일반풍속교소,풍속화유효파고야균비우측소,파향여풍향불일치.재근안태풍랑요소수지형영향교대,여외해특점불동.
Typhoon DAMREY (1210) is the strongest typhoon landed at the north of Yangtze River in the history. SWAN model driven by the Jelesnianski typhoon model wind and the NCEP wind is used to simulate the waves off Jiangsu coast. The simulated waves during Typhoon DAMREY are in good agreement with the available observations. The time evolution and spatial characteristics of typhoon waves are analyzed. Results show that the simulated maximum significant wave height is above 9m, and the wind speed and wave height on the right side of typhoon center are larger than those on the left side, and the direction of the wave accords with the wind on the right side of the typhoon center while they are not consistent on the left side. The typhoon wave near the coast is affected by the bathymetry. The distribution is different from the waves off coast.