首页> 外文会议>Coastal sediments'03: crossing disciplinary boundaries >USING GEOGRAPHIC/MARINE INFORMATION SYSTEM (GIS/MIS)FRAMEWORKS TO DETERMINE SPATIAL VARIABILITY OF BEACHSEDIMENTS AND NEARSHORE GEOMORPHOLOGY IN SUBTROPICALSOUTHEAST FLORIDA
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USING GEOGRAPHIC/MARINE INFORMATION SYSTEM (GIS/MIS)FRAMEWORKS TO DETERMINE SPATIAL VARIABILITY OF BEACHSEDIMENTS AND NEARSHORE GEOMORPHOLOGY IN SUBTROPICALSOUTHEAST FLORIDA

机译:利用地理/海洋信息系统(GIS / MIS)框架确定亚热带南部佛罗里达州海滩沉积物的空间变异性和近海地貌

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Along the subtropical barrier reef coast of southeast Florida, relativelyrnlow-energy surf zone dynamics and extreme clarity of seawater permits acquisition ofrndigital, color, aerial photographs that discriminate seabed features to at least 10 m depth.rnThe morphologic features identified from large-scale aerial photography (e.g. 1:3600)rninclude coral-algal and rock reef tracts, a wide range of sedimentary features andrnengineering works. In spite of the complexity of the coastal geomorphic system, it isrnpossible to analyze the interrelationships and feedback mechanisms betweenrnmorphological features using a remote sensing-GIS/MIS (Geographic and MarinernInformation Systems) framework and applying interpretive approaches in the analysis ofrnbeach types and nearshore morphodynamics. In an effort to ascertain the best approach tornmorphodynamic interpretation, this research compares the Wright and Short (1984)rnmodel of beach and nearshore morphological change with observed morphologies ofrncoastal segments along the lithologically controlled SE Florida coast. Calculatedrndimensionless fall velocity (?) values are combined with beach and nearshorernmorphology mapped from aerial photographs to define beach types. Omega (?) resultsrnindicate a predominance of intermediate type beaches, several process-response formsrnand unique beach-hardground-bar configurations were mapped on the aerial photographsrnand used to divide the study area into six distinct morphozones that display therncomplexity of this geomorphologic setting. Although Palm Beach County beaches arernsimilar in range to the intermediate beach types described by Wright and Short (1984),rnsome adjustments are necessary to include morphologic feedbacks that result fromrnsediment starvation and exposure of hardgrounds in southeast Florida.
机译:沿着佛罗里达州东南部的亚热带屏障礁海岸,相对低能量的冲浪带动力学和极高的海水清晰度使得可以获取数字,彩色,航拍照片,这些照片可以将海床特征区分到至少10 m的深度.rn从大规模航空摄影中识别出的形态特征(例如1:3600)包括珊瑚海藻和礁石,各种沉积特征和工程设计。尽管沿海地貌系统很复杂,但仍不可能使用遥感GIS / MIS(地理和海洋信息系统)框架来分析形态学特征之间的相互关系和反馈机制,并采用解释性方法来分析海滩类型和近岸地貌动力学。为了确定最佳的形态动力学解释方法,本研究将Wright和Short(1984)rn海滩和近岸形态变化模型与沿佛罗里达州东南部受岩性控制的沿海海岸段的形态进行了比较。计算得出的无量纲坠落速度(?)值与从航空照片映射的海滩和近岸形态相结合,以定义海滩类型。 Omega(?)结果表明主要是中型海滩,航拍照片上绘制了多种过程响应形式,并绘制了独特的海滩-硬地-杆配置,并用于将研究区域划分为六个不同的morphozones,显示了该地貌环境的复杂性。尽管棕榈滩县的海滩在范围上与Wright和Short(1984)所描述的中间海滩类型相似,但仍需要进行一些调整,以包括因沉积物饥饿和佛罗里达州东南部硬地暴露而引起的形态学反馈。

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