《浙江台风风暴潮灾害（1949-2020）》基于长期风暴潮观测预警减灾工作中积累的丰富资料，全面收集、详细分析了中华人民共和国成立以来对浙江沿海产生重要影响的风暴潮案例，图文并茂，阐述了台风风暴潮时间特征和空间分布特征，并根据潮位超警情况对台风风暴潮灾害进行了史料分类，同时介绍了浙江风暴潮灾害防御体系建设情况。
　　《浙江台风风暴潮灾害（1949-2020）》为读者了解浙江沿海风暴潮特征并开展相关研究提供了宝贵的数据资料，为提高风暴潮预警综合研判水平、发展风暴潮灾害预报技术和开展风暴潮风险评估等工作提供了科学参考依据。

　　风暴潮是由热带气旋、温带天气系统、海上飑线等风暴过境所伴随的强风和气压骤变而引起的局部海面振荡或非周期性异常升高（降低）现象，是我国沿海地区常见的海洋灾害。中国历史文献中称为海溢、海啸、海侵、大海潮等。按照引起风暴潮的大气扰动的特征，我国风暴潮大体可分为台风风暴潮和温带风暴潮两大类。台风风暴潮多发生在夏秋季节，其特点是：来势猛、速度快、强度大、破坏力强。
　　浙江省为我国沿海风暴潮灾害最严重的区域之一，又以台风风暴潮为主。历史上曾多次出现过特大台风风暴潮灾害，对浙江省的社会经济产生重大影响。据统计，1949-2020年71年间发生较明显的台风风暴潮过程139次，年平均2次，因灾死亡累计11584人；1949-2020年共有46个台风登陆浙江，平均1.5年就有一个台风在浙江登陆，登陆浙江的台风往往会造成严重风暴潮灾害。这些台风风暴潮引起沿岸增水和高潮位，导致海水漫溢堤坝、淹没沿海陆地，对浙江沿海地区生命财产造成严重威胁，经济损失巨大。1949年以来，登陆我国的超强台风5612号、0608号、1909号，强台风9417号、9711号、0216号、0414号等都在浙江省引发了特大风暴潮灾害，屡次刷新沿海潮位站历史最高潮位和最大增水记录。根据风暴潮灾后现场调查，单次登陆型强台风引发的风暴潮往往会导致海水漫过堤坝、海水入侵，使堤坝受损甚至崩溃，从而引发海水入侵内陆数千米甚至数十千米，城市内涝，良田被淹，人员伤亡等灾害，极端情况下，经济损失可超过百亿。准确模拟和评估台风风暴潮，特别是了解正面登陆台风影响下整个浙江沿海地区的风暴潮增水和高潮位分布规律，并准确评估每次台风风暴潮灾害的风险，不断提高台风风暴潮预报精度和预报的稳定度，对各级政府和有关部门做好风暴潮灾害防御与应对工作，减少台风风暴潮灾害损失有非常重要的意义。
　　本书收集整理了1949-2020年影响浙江沿海的139个台风风暴潮过程的数据资料，为全面反映浙江台风风暴潮特征及其造成的影响，本书分3章开展相关内容的辨析。第1章为“台风风暴潮灾害概述”，阐述了台风风暴潮概念、浙江省的海洋环境、历史上特大风暴潮灾害及浙江省防御体系；第2章为“浙江台风风暴潮时空特征”，阐述了风暴潮灾害评价指标、典型台风的选取、台风风暴潮时间特征及空间特征；第3章为“浙江台风风暴潮过程”，阐述了139个台风的具体情况。
　　由于时间紧，数据量大，作者水平有限，在资料整编和分析过程中，错误和疏漏之处在所难免，希望广大读者批评指正。
　　本书得到了国家自然科学基金面上项目“台风暴潮对钱塘江涌潮的影响和作用机理（51779228）”资助，在此表示感谢。

章 台风风暴潮灾害概述 ·····························································11．1 风暴潮与潮灾 ············································································31．2 浙江海洋环境 ············································································31．2．1 地理位置 ·········································································31．2．2 地形地貌 ·········································································41．2．3 气候与气象 ······································································41．2．4 岸线 ···············································································41．2．5 潮汐 ···············································································51．2．6 入海河流 ·········································································51．2．7 水下地形 ·········································································61．3 浙江历史特大风暴潮灾害 ·····························································61．4 灾害防御体系 ············································································81．4．1 海塘建设 ·········································································81．4．2 观测预报体系建设 ·····························································91．4．3 风险防控体系建设 ··························································· 11第2章 浙江台风风暴潮时空特征 ···················································· 132．1 评价指标与过程选取 ································································· 152．1．1 警戒潮位 ······································································· 152．1．2 风暴潮超警戒等级 ··························································· 182．1．3 风暴增水等级 ································································· 192．1．4 典型台风选取 ································································· 192．2 台风风暴潮时间特征分析 ··························································· 212．2．1 台风风暴潮月际分布特征 ·················································· 212．2．2 台风风暴潮年代际分布特征 ·············································· 27 2．3 台风风暴潮空间特征分析 ··························································· 282．3．1 风暴增水空间分布特征 ····················································· 282．3．2 风暴潮超警戒空间分布特征 ··············································· 32第3章 浙江台风风暴潮过程 ··························································· 353．1 超红色警戒潮位台风风暴潮 ························································ 373．2 超橙色警戒潮位台风风暴潮 ························································ 853．3 超黄色警戒潮位台风风暴潮 ·······················································1213．4 超蓝色警戒潮位台风风暴潮 ·······················································1633．5 未超警戒潮位（或未收集到潮位资料）台风风暴潮 ·························233