广东省徐闻沿海风暴潮数值模拟与淹没危险性分析 |
作者:黄宝霞1 2 胡金磊1 2 郑淑贤1 2 罗军1 2 |
单位:1. 国家海洋局南海预报中心, 广东 广州 510310; 2. 自然资源部 海洋环境探测技术与应用重点实验室, 广东 广州 510310 |
关键词:ADCIRC模型 风暴增水 耦合 淹没 |
分类号:P731.23 |
|
出版年·卷·期(页码):2022·39·第一期(39-47) |
摘要:
|
基于ADCIRC模型建立了徐闻高分辨率的风暴潮模型,并以1415号台风"海鸥"路径为基础,通过路径平移构建了一系列台风路径,模拟计算了徐闻沿海风暴增水。结果表明:徐闻东部沿岸的风暴增水最大,主要原因在于东部沿岸的独特地形特征以及该区域受到的有利台风路径影响。在上述工作的基础上,耦合海浪和天文潮的作用,计算10个不同等级下徐闻风暴潮淹没情况,计算结果显示,徐闻东部沿岸的风暴潮淹没灾害大于南部和西部沿岸。 |
Based on ADCIRC model, a high-resolution model is established to simulate the coastal storm surge along the Xuwen using a series of typhoon tracks conducted through track translation of typhoon "Kalmaegi" (1415).The results show that the maximum storm surge is along the eastern coast of Xuwen, which is mainly due to the unique topography and the favorable typhoon tracks in the area. On the basis of the above work, the storm surge inundation conditions of Xuwen under 10 different levels of minimum air pressure are calculated by coupling the effect of ocean wave and astronomical tides, which reveals that the storm surge inundation disaster along the eastern coast of Xuwen is more serious than that along the southern and western coast. |
参考文献:
|
[1] 黄锦觉. 影响徐闻的热带气旋与暴雨统计分析[J]. 广东气象, 2001(3):38-39. Huang J J. Statistical analysis of tropical cyclones and rainstorms impacted Xuwen[J]. Guangdong Meteorology, 2001(3):38-39. [2] 赵庆良, 许世远, 王军, 等. 沿海城市风暴潮灾害风险评估研究进展[J]. 地理科学进展, 2007, 26(5):32-40. Zhao Q L, Xu S Y, Wang J, et al. A review of risk assessment of storm surge on coastal cities[J]. Progress in Geography, 2007, 26(5):32-40. [3] 蒋昌波, 赵兵兵, 邓斌, 等. 北部湾台风风暴潮数值模拟及重点区域风险分析[J]. 海洋预报, 2017, 34(3):32-40. Jiang C B, Zhao B B, Deng B, et al. Numerical simulation of typhoon storm surge in the Beibu Gulf and hazardous analysis at key areas[J]. Marine Forecasts, 2017, 34(3):32-40. [4] Wang X K, Jin X L, Jia J J, et al. Simulation of water surge processes and analysis of water surge bearing capacity in Boao Bay, Hainan Island, China[J]. Ocean Engineering, 2016, 125:51- 59. [5] Quinn N, Atkinson P M, Wells N C. Modelling of tide and surge elevations in the Solent and surrounding waters:the importance of tide-surge interactions[J]. Estuarine, Coastal and Shelf Science, 2012, 112:162-172. [6] 何佩东, 左军成, 顾云碧, 等. 普陀沿海风暴潮淹没危险性评估[J]. 海洋湖沼通报, 2015(1):1-8. He P D, Zuo J C, Gu Y B, et al. Inundation risk assessment of storm surge along Putuo coastal areas[J]. Transactions of Oceanology and Limnology, 2015(1):1-8. [7] 郑国诞, 谢亚力, 胡金春, 等. 台州温岭市风暴潮淹没危险性分析[J]. 海洋预报, 2016, 33(6):40-50. Zheng G D, Xie Y L, Hu J C, et al. Inundation risk assessment of typhoon storm surge along Taizhou Wenling city[J]. Marine Forecasts, 2016, 33(6):40-50. [8] Shi X W, Qiu J F, Chen B R, et al. Storm surge risk assessment method for a coastal county in China:case study of Jinshan District, Shanghai[J]. Stochastic Environmental Research and Risk Assessment, 2020, 34(5):627-640. [9] 张敏, 罗军, 胡金磊, 等. 雷州市沿海风暴潮淹没危险性评估[J]. 热带海洋学报, 2019, 38(2):1-12. Zhang M, Luo J, Hu J L, et al. Inundation risk assessment of storm surge along Lei Zhou coastal areas[J]. Journal of Tropical Oceanography, 2019, 38(2):1-12. [10] 黄山, 朱良生. 琼州海峡附近海域2014年强台风下潮位的数值模拟与特征分析[J]. 广东水利水电, 2015(11):19-25. Huang S, Zhu L S. Numerical simulation and characteristics analysis of the water level near Qiongzhou Strait caused by 2014 strong typhoon[J]. Guangdong Water Resources and Hydropower, 2015(11):19-25. [11] 马经广, 杨武志. 台风"海鸥"与"威马逊"风暴增水的差异分析[J]. 广东水利水电, 2015(3):20-24. Ma J G, Yang W Z. Difference analysis of storm surge between typhoon Kalmaegi and Rammasun[J]. Guangdong Water Resources and Hydropower, 2015(3):20-24. [12] 熊梦捷, 章卫胜, 张金善, 等. 1522号台风"彩虹"在雷州半岛东部海域的风暴潮研究[J]. 海洋预报, 2017, 34(6):57-64. Xiong M J, Zhang W S, Zhang J S, et al. Study on strom surge of the Typhoon "Mujigae" (1522) in the East Leizhou Peninsula[J]. Marine Forecasts, 2017, 34(6):57-64. [13] 王喜年, 尹庆江, 张保明. 中国海台风风暴潮预报模式的研究与应用[J]. 水科学进展, 1991, 2(1):1-10. Wang X N, Yin Q J, Zhang B M. Research and applications of a forecasting model of typhoon surges in China Seas[J]. Advances in Water Science, 1991, 2(1):1-10. [14] Fujita T. Pressure distribution within typhoon[J]. Geophysical Magazine, 1952, 23(4):437-451. [15] 周水华, 李远芳, 冯伟忠, 等."0601"号台风控制下的广东近岸浪特征[J]. 海洋通报, 2010, 29(2):130-134. Zhou S H, Li Y F, Feng W Z, et al. Wave characteristics dominated by typhoon named ‘Pearl’[J]. Marine Science Bulletin, 2010, 29(2):130-134. [16] Blain C A, Massey T C. Application of a coupled discontinuouscontinuous galerkin finite element shallow water model to coastal ocean dynamics[J]. Ocean Modelling, 2005, 10(3/4):283-315. [17] Ris R C, Holthuijsen L H, Booij N. A third-generation wave model for coastal regions 2. Verification[J]. Journal of Geophysical Research, 1999, 104(C4):7667-7681. [18] 张海燕. 南海区台风风暴潮时空分布特征[J]. 海洋预报, 2019, 36(6):1-8. Zhang H Y. Spatio-temporal distribution of typhoon storm surge along the South China Sea coast[J]. Marine Forecasts, 2019, 36(6):1-8. |
服务与反馈:
|
【文章下载】【发表评论】【查看评论】【加入收藏】
|
|
|