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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Spatio-temporal characteristics of small-scale wave-current ripples on the Ameland ebb-tidal delta
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Spatio-temporal characteristics of small-scale wave-current ripples on the Ameland ebb-tidal delta

机译:Ameland上的小型波浪电流涟漪的时空特征eBB-TIDAL DELTA

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Ebb-tidal deltas are highly dynamic environments affected by both waves and currents that approach the coast under various angles. Among other bedforms of various scales, these hydrodynamics create small-scale bedforms (ripples), which increase the bed roughness and will therefore affect hydrodynamics and sediment transport. In morphodynamic models, sediment transport predictions depend on the roughness height, but the accuracy of these predictors has not been tested for field conditions with strongly mixed (wave-current dominated) forcing. In this study, small-scale bedforms were observed in the field with a 3D Profiling Sonar at five locations on the Ameland ebb-tidal delta, the Netherlands. Hydrodynamic conditions ranged from wave dominated to current dominated, but were mixed most of the time. Small-scale ripples were found on all studied parts of the delta, superimposed on megaripples. Even though a large range of hydrodynamic conditions was encountered, the spatio-temporal variations in small-scale ripple dimensions were relatively small (height eta approximate to 0.015 m, length lambda approximate to 0.11 m). Also, the ripples were always highly three-dimensional. These small dimensions are probably caused by the fact that the bed consists of relatively fine sediment. Five bedform height predictors were tested, but they all overestimated the ripple heights, partly because they were not created for small grain sizes. Furthermore, the predictors all have a strong dependence on wave- and current-related velocities, whereas the ripple heights measured here were only related to the near-bed orbital velocity. Therefore, ripple heights and lengths in wave-current-dominated, fine-grained coastal areas ( D50<0.25 mm) may be best estimated by constant values rather than values dependent on the hydrodynamics. In the case of the Ameland ebb-tidal delta, these values were found to be eta=0.015 m and lambda=0.11 m. (c) 2019 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd.
机译:EBB-TIDAL DELTAS是受到各种角度接近海岸的波浪和电流影响的高度动态环境。在各种尺度的其他弯曲形状中,这些流体动力学产生小尺寸弯曲床形(波纹),从而增加床粗糙度,因此会影响流体动力学和沉积物运输。在形态学模型中,沉积物传输预测取决于粗糙度高度,但这些预测器的准确性尚未对具有强烈混合(波浪电流占主导地位)强制的现场条件进行测试。在这项研究中,在荷兰Ameland EBB-TIDAL DELTA的五个地点,在现场观察到小型钻石,在荷兰的五个地点。流体动力学条件范围从主导地占据主导地位的波浪,但大部分时间都混合。在所有学习的三角洲的部分都发现了小规模涟漪,叠加在Megaripples上。即使遇到了大范围的流体动力学条件,小规模纹波尺寸的时空变化也相对较小(高度ETA近似为0.015μm,长度λ近似为0.11μm)。而且,涟漪总是高度的三维。这些小尺寸可能是由于床由相对精细的沉积物组成的事实引起的。测试了五个弯曲床位高度预测器,但它们都高估了纹波高度,部分原因是未为小粒尺寸产生。此外,预测器均具有强烈依赖波和电流相关的速度,而这里测量的纹波高度仅与近床轨道速度有关。因此,波浪电流主导的微粒沿海区域(D50 <0.25mm)中的纹波高度和长度可以通过恒定值而不是依赖于流体动力学的值最佳地估计。在Ameland EBB-TIDAL DELTA的情况下,发现这些值是ETA = 0.015米和LAMBDA =0.11μm。 (c)2019年作者。 John Wiley&Sons Ltd.出版的地球表面流程和地貌

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