首页期刊介绍通知公告编 委 会投稿须知电子期刊广告合作联系我们在线留言
 
台风“米娜”影响下的杭州湾风暴潮特征及对咸潮的影响
作者:左常圣1  黄清泽2  潘嵩1  任兴元1 
单位:1. 国家海洋信息中心, 天津 300171;
2. 自然资源部宁德海洋中心, 福建 宁德 352000
关键词:杭州湾 风暴潮 1918号台风“米娜” 非线性作用 咸潮 
分类号:P731.23
出版年·卷·期(页码):2023·40·第六期(12-20)
摘要:
基于2019年台风“米娜”风暴潮期间的实测资料,应用ADCIRC海洋模型,开展杭州湾周边海域台风风暴潮数值模拟,刻画台风期间杭州湾海域风暴增减水过程及其时空分布,并分析杭州湾风暴增减水特征以及对钱塘江咸潮入侵的影响。结果显示:芦潮港、滩浒、岱山和沈家门这4个验潮站模拟天文潮位的平均绝对误差分别为22 cm、19 cm、10 cm和14 cm,最大风暴增水的绝对误差分别为6 cm、1 cm、6 cm和7 cm,模型模拟结果良好。台风影响期间,杭州湾(湾底)的风暴增水明显大于(湾口)岛屿,滩浒站最大增水为111 cm,沈家门站最大增水为74 cm;舟山外海—杭州湾的天文潮-风暴潮的非线性作用逐渐增大,在风暴增水达到最大的过程中,各站天文潮-风暴潮的非线性作用分别为24 cm、26 cm、14 cm和4 cm;钱塘江咸潮入侵程度主要取决于径流和潮汐强度,风暴增水会在一定程度上加剧咸潮入侵灾害,在台风“米娜”风暴增水期间,钱塘江发生咸潮入侵,造成南星水厂氯度值超标41 h,因此在台风影响期间需要提前预判风暴潮对咸潮入侵的影响,做好科学应对。
Based on the observations during Typhoon "Mitag" in 2019, numerical simulation of typhoon storm surge around Hangzhou Bay has been carried out by using the ADCIRC model, to analyze the storm surge process and its characteristics in Hangzhou Bay, as well as its influence on the salt-tide intrusion of the Qiantang River. The results show that:The mean absolute errors of the simulated astronomical tide at Luchao Port, Tanxu,Daishan and Shenjiamen tide stations are 22 cm, 19 cm, 10 cm and 14 cm, respectively. The absolute errors of maximum storm surge are 6 cm, 1 cm, 6 cm and 7 cm, respectively. The storm surge in Hangzhou Bay is stronger than that of the outside islands during the typhoon. The maximum storm surge at Tanxu station is 111 cm,and that at Shenjiamen station is 74 cm. The non-linear interaction between astronomical tide and storm surge increases gradually from Zhoushan offshore to Hangzhou Bay. When the storm surge reaches its maximum, the non-linear interaction at each station are 24 cm, 26 cm, 14 cm and 4 cm, respectively. The salt-tide intrusion of Qiantang River mainly depends on runoff and tidal intensity, storm surge aggravates the salt-tide intrusion, and the salt-tide intrude the Qiantang River during Typhoon "Mitag", causing the chlorinity exceeding the limit of 41hours at the Nanxing Water Plant. It is necessary to predict the influence of storm surge on salt-tide intrusion during typhoon and to make scientific countermeasures.
参考文献:
[1] 赵昕,王晓霞,李莉.风暴潮灾害经济损失评估分析——以山东省为例[J].中国渔业经济, 2011, 29(3):91-97.ZHAO X, WANG X X, LI L. Assessment and analysis of storm surge disaster economic losses——a case of Shandong Province[J]. Chinese Fisheries Economics, 2011, 29(3):91-97.
[2] 王晓玲.我国风暴潮灾害经济风险区划[D].青岛:中国海洋大学, 2010.WANG X L. Regionalization of economic risk on storm surge disaster in China[D]. Qingdao:Ocean University of China, 2010.
[3] 马志刚,郭小勇,王玉红,等.风暴潮灾害及防灾减灾策略[J].海洋技术, 2011, 30(2):131-133.MA Z G, GUO X Y, WANG Y H, et al. Disaster of storm surge and its prevention and mitigation countermeasures[J]. Ocean Technology, 2011, 30(2):131-133.
[4] 朱军政,徐有成.浙江沿海超强台风风暴潮灾害的影响及其对策[J].海洋学研究, 2009, 27(2):104-110.ZHU J Z, XU Y C. Study on the calamity and counter-measure of the super typhoon storm surge along the Zhejiang coastal area[J].Journal of Marine Sciences, 2009, 27(2):104-110.
[5] 左常圣,王慧,李文善,等.海平面变化背景下三大河口咸潮入侵特征及变化浅析[J].海洋通报, 2021, 40(1):37-43.ZUO C S, WANG H, LI W S, et al. Characteristics and changes of salt-tide intrusion in three estuaries under the background of sea level change[J]. Marine Science Bulletin, 2021, 40(1):37-43.
[6] 陈波.北部湾台风暴潮研究现状与展望[J].广西科学, 2014(4):325-330.CHEN B. Research status and prospect of storm surge in Beibu gulf[J]. Guangxi Sciences, 2014(4):325-330.
[7] 卢益炳,马林芳. 0608号超强台风"桑美" 的主要特点和风暴潮影响特征分析[J].海洋预报, 2007, 24(4):92-96.LU Y B, MA L F. The main character of super typhoon No. 0608(SAOMAI) and characteristics analysis of its storm surge affecting[J]. Marine Forecasts, 2007, 24(4):92-96.
[8] 端义宏,朱建荣,秦曾灏,等.一个高分辨率的长江口台风风暴潮数值预报模式及其应用[J].海洋学报, 2005, 27(3):11-19.DUAN Y H, ZHU J R, QIN Z H, et al. A high-resolution numerical storm surge model in the Changjiang River Estuary and its application[J]. Acta Oceanologica Sinica, 2005, 27(3):11-19.
[9] 邓兆青,袁方超. 0908号台风"莫拉克" 风暴潮影响分析[J].海洋预报, 2011, 28(1):48-52.DENG Z Q, YUAN F C. Analysis of the storm surge due to 0908typhoon "MORAKOT"[J]. Marine Forecasts, 2011, 28(1):48-52.
[10] 姜兆敏,王如云,黄金城.风暴潮与天文潮非线性相互作用的理论分析[J].河海大学学报(自然科学版), 2004, 32(4):447-450.JIANG Z M, WANG R Y, HUANG J C. Nonlinear interaction between storm surges and astronomical tides[J]. Journal of Hohai University(Natural Sciences), 2004, 32(4):447-450.
[11] 赵永良,张延廷,陈则实.黄海风暴潮和天文潮非线性耦合作用的数值研究[J].海洋学报, 1992, 14(3):37-46.ZHAO Y L, ZHANG Y T, CHEN Z S. Numerical study of non linear interaction between storm surges and astronomical tides in the Yellow Sea[J]. Acta Oceanologica Sinica, 1992, 14(3):37-46.
[12] 周旭波,孙文心.长江口以外海域风暴潮与天文潮的非线性相互作用[J].青岛海洋大学学报, 2000, 30(2):201-206.ZHOU X B, SUN W X. The Non-linear interaction between storm surges and astronomical tides in the sea area off River Changjiang's Mouth[J]. Journal of Ocean University of Qingdao,2000, 30(2):201-206.
[13] 隋意,石洪源,钟超,等.我国台风风暴潮灾害研究[J].海洋湖沼通报, 2020(3):39-44.SUI Y, SHI H Y, ZHONG C, et al. Research on typhoon storm surge disaster in china[J]. Transactions of Oceanology and Limnology, 2020(3):39-44.
[14] 齐庆华,蔡榕硕,颜秀花.气候变化与我国海洋灾害风险治理探讨[J].海洋通报, 2019, 38(4):361-367.QI Q H, CAI R S, YAN X H. Discussion on climate change and marine disaster risk governance in the coastal China seas[J].Marine Science Bulletin, 2019, 38(4):361-367.
[15] FUJITA T. Pressure distribution in typhoon[J]. Geophysical Magazine, 1952, 23:437.
[16] MIYAZAKI M, UENO T, UNOKI S. Theoretical investigations of typhoon surges along the Japanese coast(Ⅱ) [J]. Oceanographical Magazine, 1962, 13(2):103-117.
服务与反馈:
文章下载】【发表评论】【查看评论】【加入收藏
 
 海洋预报编辑部 地址:北京海淀大慧寺路8号
电话:010-62105776
投稿网址:http://www.hyyb.org.cn
邮箱:bjb@nmefc.cn