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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >U.S. IOOS Coastal and Ocean Modeling Testbed: Hurricane‐Induced Winds, Waves, and Surge for Deep Ocean, Reef‐Fringed Islands in the Caribbean
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U.S. IOOS Coastal and Ocean Modeling Testbed: Hurricane‐Induced Winds, Waves, and Surge for Deep Ocean, Reef‐Fringed Islands in the Caribbean

机译：美国ioos沿海和海洋建模试验台：飓风诱导的风，海浪和深海，加勒比地区的礁石流苏岛浪涌

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Abstract >As part of a U.S. Integrated Ocean Observing System (IOOS) funded Coastal and Ocean Modeling Testbed (COMT), hindcasts of waves and storm surge for 2017 Hurricanes Irma and Maria are examined and compared to wave and water level gauge data in the vicinity of Puerto Rico and the U.S. Virgin Islands. The region is characterized by adjacent deep ocean water, narrow shelves, and coral reef systems providing coastal protection. The storm physics are analyzed using an unstructured grid third‐generation wave circulation coupled modeling system (ADCIRC+SWAN) with respect to tides, winds, atmospheric pressure, waves, and wave radiation stress‐induced setup. The water level response is generally dominated by the pressure deficit of the hurricanes. Wind‐driven surge is important over the shallow shelf to the east of Puerto Rico and wave‐induced setup becomes significant at locations in close proximity to the coastline. Contrary to conditions along the Gulf of Mexico shelf, geostrophically induced setup is negligible. Characteristics from a range of meteorological forcing models are assessed, and the associated errors in the hydrodynamic response are quantified. A data‐assimilated tropical planetary boundary model leads to the smallest atmospheric pressure, water level and wave property errors across both storms. Through comparisons between ADCIRC+SWAN and SLOSH‐FW (a structured grid first‐generation wave circulation coupled model), it is shown that the response to atmospheric forcing is similar; however, nearshore wave setup is smaller in SLOSH‐FW due to its coarser resolution here. Further, in addition to erroneous wind‐driven surge through depth limiting over the open ocean, numerical oscillations in the water level time series develop in SLOSH‐FW likely due to its small domain size. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“main”XML：Lang =“en”XML：ID =“JGRC23402-ABS-ABS-ABS-ABS-0001”> <标题类型=“main”> Abstract </ Title> >作为美国集成海洋观测的一部分系统（IOOS）资助的沿海和海洋建模试验台（COMT），2017年海浪和风暴飙升的飓风IRMA和Maria的Hindcasts，并与波多黎各和美国维尔京群岛附近的波和水位计数据相比。该地区的特点是邻近的深海水，狭窄的货架和提供沿海保护的珊瑚礁系统。使用非结构化电网第三代波循环耦合建模系统（ADCIRC + SWAN）对潮汐，风，大气压，波浪和波辐射应力引起的设置进行分析风暴物理学。水位响应通常由飓​​风的压力缺陷主导。风力驱动的浪涌对波多黎各以东的浅架很重要，波浪引起的设置在靠近海岸线的位置变得显着。与墨西哥湾普拉夫的条件相反，地顶尖诱导的设置可以忽略不计。评估来自一系列气象迫使模型的特征，并量化了流体动力学响应中的相关误差。数据同化的热带行星边界模型导致两个风暴中最小的大气压，水位和波属性误差。通过ADCIRC + SWAN和SLOSH-FW之间的比较（结构化电网第一代波循环耦合模型），表明对大气强制响应是相似的;然而，由于其粗糙分辨率，近岸波设置在SLOSH-FW中较小。此外，除了通过深度限制在开放的海洋上的错误的风力驱动浪涌之外，水位时间序列中的数值振荡可能由于其小域尺寸而可能在SLOSH-FW中开发。</ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共32页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Joyce B. R.&option=202" target="_blank" rel="nofollow">Joyce B. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gonzalez‐Lopez J.&option=202" target="_blank" rel="nofollow">Gonzalez‐Lopez J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Van der Westhuysen A. J.&option=202" target="_blank" rel="nofollow">Van der Westhuysen A. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang D.&option=202" target="_blank" rel="nofollow">Yang D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pringle W. J.&option=202" target="_blank" rel="nofollow">Pringle W. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Westerink J. J.&option=202" target="_blank" rel="nofollow">Westerink J. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cox A. T.&option=202" target="_blank" rel="nofollow">Cox A. T.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Civil and Environmental Engineering and Earth SciencesUniversity of Notre DameNotre Dame IN USA;</p> <p>Wood E&</p> <p>IS Met‐Ocean ServicesDartmouth Nova Scotia Canada;</p> <p>IMSG at NOAA/NWS/NCEP/Environmental Modeling CenterCollege Park MD USA;</p> <p>IMSG at NOAA/NWS/NCEP/Environmental Modeling CenterCollege Park MD USA;</p> <p>Department of Civil and Environmental Engineering and Earth SciencesUniversity of Notre DameNotre Dame IN USA;</p> <p>Department of Civil and Environmental Engineering and Earth SciencesUniversity of Notre DameNotre Dame IN USA;</p> <p>Oceanweather Inc.Stamford CT USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=storm surge model&option=203" rel="nofollow">storm surge model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wave model&option=203" rel="nofollow">wave model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hurricane Irma&option=203" rel="nofollow">Hurricane Irma;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hurricane Maria&option=203" rel="nofollow">Hurricane Maria;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=model comparison&option=203" rel="nofollow">model comparison;</a> </p> <div class="translation"> 机译：风暴浪涌模型;波模型;飓风IRMA;飓风玛丽亚;模型比较; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:22:13</span> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025579040.html">U.S. IOOS Coastal and Ocean Modeling Testbed: Hurricane‐Induced Winds, Waves, and Surge for Deep Ocean, Reef‐Fringed Islands in the Caribbean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Joyce B. 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