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Monitoring sea level rise-induced hazards along the coast of Accra in Ghana

机译:监测加纳阿克拉沿岸海平面上升诱发的危害

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Sea level rise, increased erosion and flooding threaten vulnerable coastal communities globally. Monitoring the changes in the coastal zone enables the risk levels to be detected and quantified. Such information facilitates developing sustainable policies to effectively manage hazards in the coastal zone. This study used available geospatial data to assess the physical state of the Accra coast and established ground control points that will facilitate effective monitoring of change. The data used included a bathymetric map (hard copy) with last revision in 1992, digital topographic map (2002) of the coast, 2005 orthophoto map and the geology map of Accra. The reliability of the data was determined, and the data were analysed using GIS tool. Ten concrete ground control points were established, mapped using DGPS and connected to the Ghana national coordinate system to form a network for effective monitoring in the coastal zone. The results revealed that the western region of the Accra coast has lower elevations onshore which will facilitate inundation from sea level rise. Comparing nearshore bathymetric profiles indicates that the eastern coast is deeper relative to the central and western. This will enable waves to break closer to the coast under increasing sea level rise thereby dissipating energy to facilitate sediment transport. Computed potential sediment transport rate revealed that the rate ranges between 4.1 x 10(5) and 7.2 x 10(5) m(3)/year. Using the control points established as reference points to monitor the coastal system will enable changes that can result in hazard to be detected and quantified.
机译:海平面上升,侵蚀加剧和洪水泛滥威胁着全球脆弱的沿海社区。通过监测沿海地区的变化,可以检测和量化风险水平。这些信息有助于制定可持续政策,以有效管理沿海地区的灾害。这项研究使用可用的地理空间数据来评估阿克拉海岸的物理状态,并建立了有助于有效监控变化的地面控制点。所使用的数据包括最近一次修订的测深图(硬拷贝),1992年的海岸数字地形图(2002年),2005年的正射影像图和阿克拉的地质图。确定数据的可靠性,并使用GIS工具对数据进行分析。建立了十个具体的地面控制点,使用DGPS进行了测绘,并连接到加纳国家坐标系,形成了一个有效监测沿海地区的网络。结果表明,阿克拉海岸西部地区的陆上海拔较低,这将有利于海平面上升带来的淹没。比较近岸的测深剖面表明,东部沿海地区相对于中部和西部地区更深。这将使海浪在海平面上升的情况下更靠近海岸破裂,从而消散能量以促进沉积物的运输。计算出的潜在泥沙输送速率表明,该速率介于每年4.1 x 10(5)和7.2 x 10(5)m(3)之间。使用已建立的控制点作为参考点来监视沿海系统,将可以检测和量化可能导致危害的变化。

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