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Decadal evolution of tidal flats and channels in the Outer Weser estuary, Germany

机译:德国外韦瑟河口的滩涂和河道的年代际演变

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摘要

This study focuses on the medium scale morphodynamics of the tidal flat and channel system Fedderwarder Priel, located in the Outer Weser estuary (Wadden Sea, Germany). Tidal channels and adjacent flats are highly dynamic systems whose morphologic evolution are driven by tidal, wind, and wave forcings. These coastal environments are an important ecosystem and react to changes in hydrodynamic conditions in various spatial and temporal scales. Based on annual medium-resolution digital elevation models from 1998 to 2016, we describe changes in the surface area over depth with hypsometries and use vertical dynamic trends in order to analyze and visualize the morphologic evolution of the Fedderwarder Priel and adjacent tidal channels. It is shown that several intertidal flats rise in the order of 1.3 to 5.6 cm/year. The findings indicate that the Outer Weser estuary was not in an equilibrium state for the investigated period, and tidal flats accreted with a rate exceeding mean sea level rise.
机译:这项研究的重点是位于外韦瑟河口(德国瓦登海)的滩涂和河道系统Fedderwarder Priel的中等尺度地貌动力学。潮汐通道和相邻的平坦区域是高度动态的系统,其形态演变受潮汐,风和波浪强迫的驱动。这些沿海环境是重要的生态系统,会对各种时空尺度的水力条件变化做出反应。基于1998年至2016年的年度中等分辨率数字高程模型,我们用催眠术描述了深层表面积的变化,并使用垂直动态趋势来分析和可视化Fedderwarder Priel和邻近潮汐通道的形态演变。结果表明,数个潮间带单位以每年1.3至5.6厘米的速度上升。调查结果表明,在调查期间外韦瑟河口未处于平衡状态,潮滩以超过平均海平面上升速度的速度增加。

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