Bed forms under the combined action of waves and wind-driven currents in the remote foreshore of the non-tidal sea

IF 2.6 3区 地球科学 Q2 OCEANOGRAPHY
Magdalena Stella-Bogusz
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引用次数: 0

Abstract

The paper presents a prediction of bed form parameters (length and height) in the remote foreshore of the non-tidal sea. The study site is located in the south Baltic region, near the Coastal Research Station (CRS) in Lubiatowo, Poland (ca. 1–2 Nm off the shoreline at depths of around 16–20 m). The study site is an area with hydrodynamics and lithodynamics typical of the south Baltic coast, built of fine sands. Predictions are based on numerical modelling with an input of measured data. Numerical modelling uses assumptions of specific relations of sand wave height and length with shear stress, grain size, kinematic viscosity, or storm event frequency. To establish these relations for the study area, wave, sea temperature and wind data were collected near CRS Lubiatowo. To verify the predictions made in this research, bathymetric data from a field survey in the study area was used. The results show that the flow is mostly current-dominated. Sand waves formed by hydrodynamic conditions in this area have a steepness of 0.01 to 0.02, a length of 40 to 70 m and a height of 0.6 to 2.3 m.

在非潮汐海的远前海岸,在波浪和风力驱动的洋流的共同作用下形成了海床
本文提出了一种预测非潮汐海远前滩河床形态参数(长度和高度)的方法。研究地点位于波罗的海南部地区,靠近波兰Lubiatowo的海岸研究站(CRS)(距离海岸线约1-2海里,深度约16-20米)。研究地点是波罗的海南部海岸典型的流体动力学和岩石动力学区域,由细沙建成。预测是基于数值模拟和输入测量数据。数值模拟使用沙波高度和长度与剪切应力、粒度、运动粘度或风暴事件频率的特定关系的假设。为了建立研究区域的这些关系,在CRS Lubiatowo附近收集了波浪、海温和风的数据。为了验证本研究中的预测,使用了研究区域野外调查的水深数据。结果表明:流动以电流为主;该地区水动力条件形成的沙波陡度为0.01 ~ 0.02,长度为40 ~ 70 m,高度为0.6 ~ 2.3 m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Oceanologia
Oceanologia 地学-海洋学
CiteScore
5.30
自引率
6.90%
发文量
63
审稿时长
146 days
期刊介绍: Oceanologia is an international journal that publishes results of original research in the field of marine sciences with emphasis on the European seas.
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