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HISTORICAL SHORELINE CHANGES AND MORPHODYNAMICS OF PARRAMORE ISLAND, VIRGINIA (1852-2006)

机译:弗吉尼亚帕雷玛岛的历史海岸线变化和形态学性(1852-2006)

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摘要

Using National Ocean Service topographic sheets and global positioning system shoreline position surveyss historical shoreline changes of Parramore Island, Virginia, are quantified between 1852 and 2006 to address long- and short-term trends in shoreline movement Quantitative analyses of twelve high water line (shoreline) positions indicate the shoreline is retreating at increasing rates in the short term (decadal) when compared with long-term trends (centennial). In particular, the behavior of the outer shoreline changed from clockwise rotational instability to sustained retreat Parramore's entire outer shoreline (Cells 3, 4, and 5) experienced a retreat rate of -3.6 m/yr over the long term (1852-2006) and -8.8 m/yr over the short term (1998-2006). The short-term rate changes indicate that the processes controlling shoreline trends, e.g., overwash to the south and inlet dynamics to the north, have intensified and/or changed relative to the long-term.
机译:使用国家海洋服务地形表和全球定位系统海岸线位置调查帕雷莫尔岛,弗吉尼亚岛的历史海岸线变化在1852年至2006年之间量化,以解决十二高水线(海岸线)的海岸线运动定量分析的长期和短期趋势。与长期趋势(百年)相比,位置表明,在短期(Decadal)中,海岸线正在撤回速度下降。特别地,外部海岸线的行为从顺时针旋转不稳定性变为持续的退缩剖腹产的整个外部海岸线(电池3,4和5)在长期(1852-2006)中经历了-3.6米/年的后退率。短期内--8.8米/年(1998-2006)。短期汇率变化表明,控制海岸线趋势的过程,例如北方的南部和入口动力学,相对于长期进行加剧和/或改变。

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