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浙江沿海潜在区域地震海啸风险分析

毛献忠 祝倩 Wei Yong

毛献忠, 祝倩, Wei Yong. 浙江沿海潜在区域地震海啸风险分析[J]. 海洋学报, 2015, 37(3): 37-45. doi: 10.3969/j.issn.0253-4193.2015.03.004
引用本文: 毛献忠, 祝倩, Wei Yong. 浙江沿海潜在区域地震海啸风险分析[J]. 海洋学报, 2015, 37(3): 37-45. doi: 10.3969/j.issn.0253-4193.2015.03.004
Mao Xianzhong, Zhu Qian, Wei Yong. Risk analysis of potential regional earthquake tsunami on the coast of Zhejiang Province[J]. Haiyang Xuebao, 2015, 37(3): 37-45. doi: 10.3969/j.issn.0253-4193.2015.03.004
Citation: Mao Xianzhong, Zhu Qian, Wei Yong. Risk analysis of potential regional earthquake tsunami on the coast of Zhejiang Province[J]. Haiyang Xuebao, 2015, 37(3): 37-45. doi: 10.3969/j.issn.0253-4193.2015.03.004

浙江沿海潜在区域地震海啸风险分析

doi: 10.3969/j.issn.0253-4193.2015.03.004
基金项目: 国家自然科学基金项目(41176001);深圳市科技项目(GJHS20120702112942334);深圳市近海动力环境演变重点实验室(ZDSY20130402163735964)。

Risk analysis of potential regional earthquake tsunami on the coast of Zhejiang Province

  • 摘要: 采用COMCOT海啸模型建立三重网格模型模拟了2011年3月11日日本东北部9.0级地震引发的海啸发生、发展以及在我国东南沿海传播过程。震源附近浮标站以及浙江沿海的潮位站实测资料验证结果显示,大部分监测站首波到达时间和海啸波的计算值相差在15%以内,表明模型可较好的模拟海啸在计算域内的传播过程。研究表明日本南海海槽、冲绳海槽以及琉球海沟南部是影响浙江沿海主要的区域潜在震源,通过情景计算分别模拟3个潜在震源9.1级、8.0级和8.7级地震引发的海啸对浙江沿海的海啸风险,计算结果表明,海啸波产生后可在3~8 h内传至浙江省沿岸,海啸波达1~3 m,最大可达4 m,此时浙江沿岸面临Ⅲ~Ⅳ级海啸风险,达到淹没至严重淹没等级。
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  • 收稿日期:  2014-04-11

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