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A NON-HYDROSTATIC NUMERICAL MODELLING OF EXCHANGE FLOWS

机译:交换流的非静力学数值模拟

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摘要

Stratified exchange flows are investigated by a three-dimensional, non-hydrostatic, numerical model with a free surface. The model is based on 3D Reynolds-averaged Navier-Stokes equations under the Boussinesq assumption. The model equations are written in a generalized vertical coordinate system and with orthogonal curvilinear horizontal coordinates. A mode splitting technique, decomposition of pressure and velocity fields into hydrostatic and non-hydrostatic components and sequential calculation of these components are the base of numerical algorithm of the model. The model was tested against a laboratory experiment on the exchange flow through long and narrow strait and was applied to simulate the water exchange through the Strait of Dardanelles. It reproduces the complicated three-dimensional structures of currents in the Dardanelles. It also shows that mixing plays a crucial role in maintaning the observed exchange flow between the Aegean and Marmara seas.
机译:通过具有自由表面的三维非静液压数值模型研究了分层交换流量。该模型基于Boussinesq假设下的3D雷诺平均Navier-Stokes方程。模型方程写在广义的垂直坐标系中,并具有正交的曲线水平坐标。该模型的数值算法的基础是一种模式分裂技术,将压力和速度场分解为静水和非静水分量以及这些分量的顺序计算。该模型通过实验室实验对通过狭窄和狭窄海峡的交换水进行了测试,并被用于模拟通过达达尼尔海峡海峡的水交换。它再现了达达尼尔海峡中复杂的水流三维结构。它还表明,混合在维持观察到的爱琴海与马尔马拉海之间的交换流量中起着至关重要的作用。

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