海洋科学
海洋科學
해양과학
MARINE SCIENCES
2013年
11期
95-102
,共8页
风暴增水%圆对称风场%模型风场%流入角
風暴增水%圓對稱風場%模型風場%流入角
풍폭증수%원대칭풍장%모형풍장%류입각
storm surge%circular symmetric wind field%mold wind field%inflow angle
对0814号台风进行了增水模拟,以及建立一个适合0814号台风类型的模型风场,用于将来的风暴潮模拟。文章使用香港天文台数据进行增水模拟验证,在模式未考虑气压、远程天气、径流等因素对增水作用下,模式将误差控制在20%以内,据已有研究结果表明,模式具有一定的准确性。在建立风场模型中,首先,通过对比已有圆对称风场模型,确认 Dual 模型更为合理;其次利用藤田公式对参数化流入角进行修正,对风场的流向与温度、强度建立联系,并讨论流入角度变化对增水影响;再次,通过叠加移动风场,获得右侧风速偏大的风场,以及讨论其对增水的影响;最后,尝试添加背景风场,并对比添加前后增水变化,发现最大增水点附近增水降低,而台风中心附近和外围区域增水增加。本文认为公式叠加背景风场更加合理,选取背景风场数据最好不包含台风信息。此风场的建立主要为研究南海风暴潮变化机理及后报做铺垫。
對0814號檯風進行瞭增水模擬,以及建立一箇適閤0814號檯風類型的模型風場,用于將來的風暴潮模擬。文章使用香港天文檯數據進行增水模擬驗證,在模式未攷慮氣壓、遠程天氣、徑流等因素對增水作用下,模式將誤差控製在20%以內,據已有研究結果錶明,模式具有一定的準確性。在建立風場模型中,首先,通過對比已有圓對稱風場模型,確認 Dual 模型更為閤理;其次利用籐田公式對參數化流入角進行脩正,對風場的流嚮與溫度、彊度建立聯繫,併討論流入角度變化對增水影響;再次,通過疊加移動風場,穫得右側風速偏大的風場,以及討論其對增水的影響;最後,嘗試添加揹景風場,併對比添加前後增水變化,髮現最大增水點附近增水降低,而檯風中心附近和外圍區域增水增加。本文認為公式疊加揹景風場更加閤理,選取揹景風場數據最好不包含檯風信息。此風場的建立主要為研究南海風暴潮變化機理及後報做鋪墊。
대0814호태풍진행료증수모의,이급건립일개괄합0814호태풍류형적모형풍장,용우장래적풍폭조모의。문장사용향항천문태수거진행증수모의험증,재모식미고필기압、원정천기、경류등인소대증수작용하,모식장오차공제재20%이내,거이유연구결과표명,모식구유일정적준학성。재건립풍장모형중,수선,통과대비이유원대칭풍장모형,학인 Dual 모형경위합리;기차이용등전공식대삼수화류입각진행수정,대풍장적류향여온도、강도건립련계,병토론류입각도변화대증수영향;재차,통과첩가이동풍장,획득우측풍속편대적풍장,이급토론기대증수적영향;최후,상시첨가배경풍장,병대비첨가전후증수변화,발현최대증수점부근증수강저,이태풍중심부근화외위구역증수증가。본문인위공식첩가배경풍장경가합리,선취배경풍장수거최호불포함태풍신식。차풍장적건립주요위연구남해풍폭조변화궤리급후보주포점。
We simulated the surge and constructed a wind filed for 0814 Typhoon, which can be used for storm surge research later. We verified the surge simulation by data from Hong Kong Observatory. The results showed that when neglecting the effects of pressure and remote atmospheric, the simulation was satisfying and model error was within 20 percent. After researching circularly symmetric wind model, we found the Dual wind was the best. Then with the Fujita Formula we improved the parameterization of inflow angle, which connected inflow angle with temperature and wind velocity. We also discussed the effects of inflow angle’s change on surge. After adding mov-ing wind field, we established a new wind field, in which the right wind velocity was larger and then also discussed its effects on surge. Finally, we added the background wind field, which reduced the surge around the maximum surge point and also increased surge near the center of typhoon. Through this study, it was not appropriate to con-sider the wind filed which contains information about the typhoon’s background wind field. In this situation, adding wind fields by formulas was a better choice.