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首页> 外文期刊>Natural hazards and earth system sciences >Hydrodynamic modelling of coastal seas: the role of tidal dynamics in the Messina Strait, Western Mediterranean Sea
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Hydrodynamic modelling of coastal seas: the role of tidal dynamics in the Messina Strait, Western Mediterranean Sea

机译:沿海海洋的流体动力学模拟:潮汐动力学在西地中海墨西拿海峡中的作用

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摘要

This work explores the importance of considering tidal dynamics when modelling the general circulation in the Messina Strait, a narrow passage connecting the Tyrrhenian and the Ionian subbasins in the Western Mediterranean Sea. The tides and the induced water circulation in this Strait are among the most intense oceanographic processes in the Mediterranean Sea. The quantification of these effects can be particularly relevant for operational oceanographic systems aimed to provide short-term predictions of the main hydrodynamics in the Western Mediterranean subbasins. A numerical approach based on the use of a high-resolution hydrodynamic model was followed to reproduce the tides propagation and the wind-induced and thermohaline water circulation within the Strait and in surrounding areas. A set of numerical simulations was carried out to quantify the role of the Strait dynamics on the larger-scale water circulation. The obtained results confirmed the importance of a correct representation of the hydrodynamics in the Messina Strait even when focusing on predicting the water circulation in the external sea traits. In fact, model results show that tidal dynamics deeply impact the reproduction of the instantaneous and residual circulation pattern, waters thermohaline properties and transport dynamics both inside the Messina Strait and in the surrounding coastal and open waters.
机译:这项工作探索了在对墨西拿海峡的总体环流进行建模时考虑潮汐动力学的重要性,墨西拿海峡是一条连接西地中海第勒尼安海盆地和爱奥尼亚海盆地的狭窄通道。海峡中的潮汐和引起的水循环是地中海最强烈的海洋学过程之一。这些影响的量化对于旨在为西地中海子盆地的主要水动力提供短期预测的可操作海洋学系统尤其重要。遵循了基于高分辨率水动力模型的数值方法,以再现海峡内及周围地区的潮汐传播以及风诱发和热盐分水的循环。进行了一组数值模拟,以量化海峡动力学在大规模水循环中的作用。所获得的结果证实了即使专注于预测外部海洋特征中的水循环,也必须正确表示墨西拿海峡中的水动力的重要性。实际上,模型结果表明,潮汐动力学深刻地影响了墨西拿海峡内部以及周围沿海和开阔水域的瞬时和残留循环模式,水域热盐特性和运移动力学的再现。

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