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1Tidal Asymmetry Changes in a Shallow Mud Estuary by a Restoration Project显示文摘The tidal asymmetry-induced siltation below tidal barriers is a worldwide problem that restricts regional socio-economic and environmental development. The hydrodynamic processes of the small mud estuary also feature a high uncertainty after estuary restoration measures. In this study, a hydrodynamic model based on the MIKE21 is used to quantify the responses of tidal asymmetry to a two-phase restoration project in Shuanglong Estuary, Bohai Bay, China. According to the numerical modeling results, the tidal flat removal in the upper estuary(first-phase restoration) induces the flood asymmetry switching to the ebb asymmetry in unrestored reach but enhances flood asymmetry in widening restored reach. Although the tidal asymmetry reverts to flood-dominated pattern after full restoration over the estuary, the imbalance between flood and ebb velocities is relieved. A possible net sediment transport pattern based on a comparison of dominant asymmetric current and actual sediment transport period shows net sediments in the upper estuary and inlet transport seaward and landward, respectively, in the first-phase restoration, whereas landward net sediment transport occurs in the whole estuary under the second-phase restoration scenario. Given these results, we assume that a switch from the flood-dominated estuary to ebb-dominated estuary can be caused by redesigning the cross-sectional profile. The quantitative comparison of Lagrangian residual currents also implies that a channel–shoal structure rather than a flat bathymetry can promote the mass transport. Therefore, reshaping the channel–tidal flat system in restoration projects can prevent the sedimentation of the estuary and improve the water environment.LIANG Huidi KUANG Cuiping GU Jie MA Yue CHEN Kuo LIU Xu 2019Journal of Ocean University of China2019,18,2:2
2基于GEE的东海渔场长时间序列环境分析显示文摘地球环境变化分析研究中,大尺度长时间序列遥感是研究的数据基础。Google Earth Engine(GEE)借助谷歌公司高性能的并行计算与高效率的数据管理技术,为科研人员提供在线可视化计算和分析处理的云平台。文章利用GEE提取MODIS-Terra的L3SMI的海表温度和叶绿素数据,根据东海渔场范围计算20年的年平均温度和叶绿素。通过分析表明:我国东海的渔场的年平均海表温度由北向南逐渐升高,近海渔场年平均温度在20~26℃,外海渔场年平均温度在22~28℃,外海年平均温度高于近海。东海的渔场年平均叶绿素浓度由北向南逐渐降低,近海渔场年平均叶绿素浓度在0.8~4 mg/m3,外海渔场年平均叶绿素浓度在0.1~1.2 mg/m3,外海渔场低于近海渔场。张胜茂 常卫东 王斐 杨胜龙 2021电脑与信息技术2021,29,1:1
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