里约热内卢海岸海洋水热力学模拟的稳定有限元模型

C. Carbonel, A. Galeão
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引用次数: 7

摘要

本文建立了沿海海洋环流的稳定时空Petrov-Galerkin有限元模型。在空间和时间上采用连续线性插值,并采用三角形单元的空间非结构化网格。为了模拟海洋的水热动力学行为,提出了一个重力简化模型。该模型求解了运动和连续流体动力学方程以及控制上层热交换的温度平流-扩散输运方程。该模式用于评价巴西里约热内卢州沿海水域的主要动力特征,即:冷羽流、沿海喷流和暖水湾的影响。通过数值实验,重点分析了海岸上升流现象的典型观测事件及其与现有海岸海湾和近海条件的相互作用。这些实验处理了一系列理想化的东北风场强迫模式,显示了与海岸线配置相关的风场水平结构的解依赖。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A stabilized finite element model for the hydrothermodynamical simulation of the Rio de Janeiro coastal ocean
In this paper, a stabilized space-time Petrov-Galerkin finite element model of coastal ocean circulation is derived. Continuous linear interpolation in space and time is employed and a spatial unstructured mesh of triangular elements is used. To simulate the hydro-thermodynamical ocean behaviour a gravity reduced model is proposed. This model solves the motion and continuity hydrodynamic equations coupled with the advection-diffusion transport equation for temperature which governs the heat exchanges in the upper layer. The model is used to evaluate the main dynamical features of the coastal waters of the Rio de Janeiro State, namely: cold plumes, coastal jets and the influence of the warmer water bays. Numerical experiments are performed to highlight the typical observed events of coastal upwelling phenomena and their interaction with the existing coastal bays and the offshore conditions. Such experiments deal with a series of idealized northeast wind field forcing patterns, showing the solutions dependence on the horizontal structure of the wind fields in relation to the coastline configuration.
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