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作 者:Yu Yao Baobao Zhou Zhongwei Zhao Xianjin Chen Long Chen
机构地区:[1]School of Hydraulic and Environmental Engineering,Changsha University of Science and Technology,Changsha 410114,China [2]Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China [3]Key Laboratory of Water-Sediment Sciences and Water Disaster Prevention of Hunan Province,Changsha 410114,China
出 处:《Acta Oceanologica Sinica》2023年第7期41-50,共10页海洋学报(英文版)
基 金:The National Natural Science Foundation of China under contract Nos 51979013 and 51909013;the National Key Research and Development Program of China under contract Nos 2021YFC3100502 and 2021YFB2601105;the Hainan Provincial Natural Science Foundation of China under contract No.421QN0978.
摘 要:The persistence and habitability of coral reef islands in future extreme oceanographic conditions has received increasing attention in the recent decade,concerning that the sea level rise(SLR)and more frequent and intense storms in the context of global climate change are expected to destabilize those islands.Here,we conduct a set of wave-flume laboratory experiments focusing on the morphodynamic change of reef islands to varying ocean forcing conditions(wave height and SLR).Subsequently,a phase-resolving XBeach numerical model is adopted to simulate the monochromatic wave process and its associated sediment dynamics.The adopted model is also firstly validated by laboratory experimental results as reported in this study.It is then used to examine the impacts of island morphological factors(island width,island height,island location and island side slope)on the island migration.The combined laboratory/physical and numerical experiment outputs suggest that reef islands can accrete vertically in response to the sea level rise and the increased storminess.
关 键 词:coastal morphodynamics sea level rise reef island wave-flume experiment XBeach model
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