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首页> 外文期刊>Archives of Hydro-engineering and Environmental Mechanics >Wind Influence on the Formation of Nearshore Currents in the Southern Baltic: Numerical Modelling Results
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Wind Influence on the Formation of Nearshore Currents in the Southern Baltic: Numerical Modelling Results

机译:风对波罗的海南部近海海流形成的影响:数值模拟结果

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A two-dimensional numerical model was used for a simulation of vertical average longshore currents generated by both wind friction and wind-wave action in the nearshore zone. The modelling domain includes the southern part of the Baltic Proper (all boundaries were closed). Wind, uniform in space and varying in time, was the only forcing in the model. The correlation coefficient higher than 0.8 was obtained by model calibration versus the field measurements of currents conducted at the Lubiatowo field station (southern Baltic) during about 1.5 months in 2006. Comparative simulations of total currents including both wind-induced drift and wave components, and of total currents including only a wind-induced drift component, showed that the input of the drift component into currents in the nearshore zone is greater than commonly believed. Wind-induced drift strongly dominates outside the zone of wave transformation, and its input into the total resulting currents remains noticeable even in a zone between the shoreline and the depth of the first wave breaking. Thus, wind-induced drift constitutes up to 50% of the resulting longshore currents for longshore winds and no less than 20% of the longshore component of currents for winds at 45 degrees to the longshore direction.
机译:使用二维数值模型来模拟近岸区域的风摩擦和风浪作用所产生的垂直平均沿岸电流。建模领域包括波罗的海南部的南部(所有边界均封闭)。在空间中均匀且随时间变化的风是模型中唯一的强迫。通过模型校准获得的相关系数高于0.8,相对于2006年大约1.5个月在Lubiatowo野外站(波罗的海南部)进行的电流实地测量得出的总电流的比较模拟,包括风致漂移和波分量,以及仅包括风致漂移分量的总电流的总和表明,漂移分量输入近海区域的电流要比通常认为的要大。由风引起的漂移在波浪变换带以外的地方占主导地位,即使在海岸线和第一次波浪破碎深度之间的区域中,其向总合流的输入仍然很明显。因此,由风引起的漂移占到了沿岸风向所产生的沿岸风流的50%,并且不小于沿沿岸向45度的风向所产生的沿岸风流的沿岸风分量的20%。

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