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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >A new high-resolution unstructured grid finite volume Arctic Ocean model (AO-FVCOM): An application for tidal studies
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A new high-resolution unstructured grid finite volume Arctic Ocean model (AO-FVCOM): An application for tidal studies

机译:一种新的高分辨率非结构化网格有限体积北冰洋模型(AO-FVCOM):潮汐研究的应用

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摘要

A spherical coordinate version of the unstructured grid 3-D FVCOM (finite volume coastal ocean model) has been applied to the Arctic Ocean to simulate tides with a horizontal resolution ranging from 1 km in the near-coastal areas to 15 km in the deep ocean. By accurately resolving the irregular coastlines and bathymetry in the Arctic Ocean coastal regions, this model reproduces the diurnal (K_1 and 0_1) and semidiurnal (M_2 and S_2) tidal wave dynamics and captures the complex tidal structure along the coast, particularly in the narrow straits of the Canadian Archipelago. The simulated tidal parameters (harmonic constituents of sea surface elevation and currents) agree well with the available observational data. High-resolution meshes over the continental shelf and slope capture the detailed spatial structure of topographic trapped shelf waves, which are quite energetic along the Greenland, Siberia, and Spitsbergen continental slope and shelf break areas. Water stratification influences the vertical distribution of tidal currents but not the water transport and thus tidal elevation. The comparison with previous finite difference models suggests that horizontal resolution and geometric fitting are two prerequisites to simulate realistically the tidal energy flux in the Arctic Ocean, particularly in the Canadian Archipelago.
机译:非结构化网格3-D FVCOM(有限体积沿海海洋模型)的球坐标版本已应用于北冰洋,模拟了潮汐,其水平分辨率范围从近沿海地区的1 km到深海地区的15 km 。通过精确地解决北冰洋沿海地区的不规则海岸线和水深,该模型再现了日(K_1和0_1)和半日(M_2和S_2)潮汐动力学,并捕获了沿海特别是狭窄海峡中的复杂潮汐结构。加拿大群岛。模拟的潮汐参数(海面高程和洋流的谐波成分)与可用的观测数据非常吻合。大陆架和斜坡上的高分辨率网格捕获了被困的地形波的详细空间结构,这些格网在格陵兰,西伯利亚和斯匹次卑尔根大陆斜坡和架折处非常活跃。水的分层影响潮汐流的垂直分布,但不影响水的运输,因而不影响潮汐的升高。与以前的有限差分模型的比较表明,水平分辨率和几何拟合是现实地模拟北冰洋,特别是加拿大群岛中的潮汐能通量的两个先决条件。

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