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Forcing mechanisms and hydrodynamics in Loch Linnhe, a dynamically wide Scottish estuary

机译:动态宽广的苏格兰河口林赫湖的强迫机制和流体动力学

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Hydrodynamic conditions in Loch Linnhe, a dynamifcally wide estuary on the west coast of Scotland, are primarily influenced by wind forcing, freshwater input, and tides. Winds in the region are orographically steered along the axis of the estuary due to surrounding mountains. A large rainfall catchment area results in a large freshwater inflow into Loch Linnhe which in turn produces low salinity waters at the head of the estuary. This, combined with a connection to the open sea with coastal salinities, leads to salinity gradients in the horizontal and vertical. Even though a range of observational programmes have focussed on Loch Linnhe, the literature still lacks an evaluation of its physical dynamics. Here we present a first description of the hydrodynamics in Loch Linnhe based on observations. Wind stress predominantly influences the surface layer, especially at low frequencies and with a stronger influence than tides during neap tides. The buoyancy-driven flow due to the large river runoff influences the circulation independent of wind stress. Seasonal (spring, autumn) and interannual (2011, 2012) variability of water masses occur especially in the surface layer. Tides are dominated by the semi-diurnal constituent M-2 with tidal ellipses aligned in the along-estuary direction and a stronger influence during spring tides compared to wind. An evaluation of dimensionless numbers reveal laterally and vertically sheared exchange flows. Compared to other Scottish estuaries Loch Linnhe is wide enough to be influenced by the Earth's rotation and demonstrates an enhanced freshwater outflow along its north-western coast as the freshwater is diverted to the right in the direction of the flow. These observed patterns are important for the sustainable environmental management of this socio-economically valuable region, e.g. through their relevance to aquaculture pathogen transmission patterns. A thorough understanding of the dynamics of the system is essential for a successful evidence-based marine planning framework. Crown Copyright (C) 2017 Published by Elsevier Ltd. All rights reserved.
机译:苏格兰西海岸一个充满活力的河口林湖(Loch Linnhe)的水动力条件主要受到强迫,淡水输入和潮汐的影响。由于周围有群山,该地区的风在地形上沿河口的轴线转向。大的降雨集水区导致大量的淡水流入Linnhe湖,这反过来又在河口顶部产生了低盐度的水。这加上与沿海盐度与公海的联系,导致水平和垂直盐度梯度。即使一系列的观测计划都集中在林赫湖上,但文献仍然缺乏对其物理动力学的评估。在这里,我们基于观察结果,对林湖的水动力学进行了首次描述。风应力主要影响表面层,尤其是在低频时,并且在小潮期间比潮汐影响更大。由于大的河流径流而产生的浮力驱动的流量独立于风应力影响了环流。水团的季节性(春季,秋季)和年度间(2011年,2012年)都发生变化,尤其是在表层。潮汐主要由半日组成部分M-2所占据,潮汐椭圆沿河口方向排列,与春季相比,春季潮汐的影响更大。无量纲数的评估揭示了横向和垂直剪切的交换流量。与其他苏格兰河口相比,Linnhe宽得足以受到地球自转的影响,并且随着淡水沿水流方向向右转移,沿西北海岸的淡水流出量有所增加。这些观察到的模式对于这个具有社会经济价值的地区(例如通过它们与水产养殖病原体传播方式的相关性。对系统动态的透彻了解对于成功的基于证据的海洋规划框架至关重要。 Crown版权所有(C)2017,由Elsevier Ltd.出版。保留所有权利。

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