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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Numerical simulation of the tidal propagation in the coastal region of Santos (Brazil, 24 degrees S 46 degrees W)
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Numerical simulation of the tidal propagation in the coastal region of Santos (Brazil, 24 degrees S 46 degrees W)

机译:桑托斯沿海地区(巴西,南纬24度46度)潮汐传播的数值模拟

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A sigma vertical co-ordinate model was implemented for the coastal region of Santos (Brazil, 24degreesS 46degreesW), aiming at high-resolution barotropic tidal simulations. On a grid of 120 x 80 cells and spacing of about I km, tidal elevations due to the nine principal constituents were specified at the open boundaries, based on a model of the shelf. The coastal model results were compared to observations and harmonic predictions in the Port of Santos. Tidal analyses of time series relative to 5527 wet points, with 696 hourly results of elevations and surface currents each, generated maps of the co-tidal lines and axes of the current ellipses, which numerical values were compared to harmonic constants of some coastal stations. The obtained maps indicate the main characteristics of the tides in the coastal region of Santos, such as the areas of amplification and main propagation directions. The model results generated maps of the potential, kinetic and total energies associated to the tides. Residual depth-mean currents show tidal eddies related to coastal geometry and bottom topography. Vertical profiles of the tidal currents have nearly constant intensities and directions along the vertical, from the surface to the top of the bottom layer. The implemented modeling may be used for operational predictions of tides and tidal currents in the study area, especially when considering grid nestings in the shallow inner regions. (C) 2003 Elsevier Ltd. All rights reserved. [References: 32]
机译:针对高分辨率的正压潮汐模拟,在桑托斯沿海地区(巴西,24°S 46°W)实施了sigma垂直坐标模型。在一个120 x 80单元的网格和大约1 km的间距上,基于架子模型,在开放边界处指定了由9种主要成分引起的潮汐高程。将沿海模型的结果与桑托斯港的观测结果和谐波预测进行了比较。相对于5527个湿点的时间序列的潮汐分析,每个小时都有696个小时的高程和地面水流结果,生成了共潮线图和当前椭圆轴的图,并将这些图的值与某些沿海站点的谐波常数进行了比较。所获得的地图显示了桑托斯沿海地区的潮汐的主要特征,例如放大区域和主要传播方向。模型结果生成了与潮汐相关的势能,动能和总能的映射。剩余深度平均流显示出与海岸几何和底部地形有关的潮汐涡。从底层的表面到顶层,潮流的垂直剖面沿垂直方向具有几乎恒定的强度和方向。所实现的模型可用于研究区域内潮汐和潮流的运行预测,尤其是考虑浅内部区域的网格嵌套时。 (C)2003 Elsevier Ltd.保留所有权利。 [参考:32]

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