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Tidally generated shelf waves off the western Iberian coast

机译:潮汐产生的架子波在伊比利亚西部海岸附近

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摘要

A high-resolution finite element model of barotropic tides in the Iberian Atlantic shelf is presented. The model accurately reproduces available tidal data, with average amplitude discrepancies at 12 Atlantic stations below 3% and 15% for semi-diurnal and diurnal tides, respectively. The accuracy of the model simulations is supported also by a qualitative comparison with velocity data. The model results are used to examine the generation of shelf waves by diurnal tides off the western Portuguese coast. Shelf waves in this area are responsible for large diurnal currents, which can exceed semi-diurnal currents by an order of magnitude. Numerical experiments show that these shelf waves can be generated by obstacles perpendicular to the coastline, and are enhanced in the presence of wide and shallow shelves and steep continental slopes. Along the Portuguese coast, the Tagus plateau is responsible for most of the shelf wave generation. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 39]
机译:提出了伊比利亚大西洋大陆架正压潮的高分辨率有限元模型。该模型准确地再现了可用的潮汐数据,半日潮和日潮的12个大西洋站的平均幅度差异分别低于3%和15%。与速度数据的定性比较也支持模型仿真的准确性。模型结果被用来检验葡萄牙西部沿海的日潮产生的架波。该区域的搁板波造成大的日潮流,可能比半日潮流大一个数量级。数值实验表明,这些架子波可以由垂直于海岸线的障碍物产生,并在宽而浅的架子和陡峭的大陆坡的存在下得到增强。沿着葡萄牙海岸,塔霍高原是大部分架子波产生的原因。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:39]

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