NUMERICAL MODELS’ APPLICATION FOR MORPHODYNAMICS ASSESSMENT OF CLIMATE CHANGE IMPACTS IN THE MINHO RIVER ESTUARY

Willian Melo, J. Pinho, I. Iglesias, A. Bio, P. Avilez-Valente, Ana Gomes, José Vieira, L. Bastos, F. Veloso-Gomes
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Abstract

The knowledge of physical, biological, and chemical estuarine processes and how they are affected by climate change conditions is essential for improving estuarine management. A common methodological approach for studying these complex processes is based on the implementation of numerical models supported by field data as bathymetry, sediment characteristics, flow discharges, current velocities, and sea water levels. This work is based on the implementation of a numerical model of the Minho River estuary using the Delft3D software. This model is able to simulate hydrodynamic and morphodynamic processes for different time scales. It was calibrated using the OpenDA tool, which automatically determines some of the models’ parameters, such as the tidal constituents and the roughness coefficient, aiming to minimize the error between observed data and simulated results. Different scenarios were considered to assess the effects of climate change, according to the 5th Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). Results showed that the elevation in the estuary mouth can reach 77 cm, depending on the considered scenario. It was also determined that floods are the main sediment transport driver along the estuary, intensifying the accretion processes. Furthermore, the sea-level rise reduces the amount of transported sediments to the coastal platform, increasing the erosion risk in this area and increasing the accretion inside the estuary.
数值模式在米尼奥河河口气候变化影响形态动力学评价中的应用
了解河口的物理、生物和化学过程以及它们如何受到气候变化条件的影响,对于改善河口管理至关重要。研究这些复杂过程的一种常用方法是基于数值模型的实施,这些模型由测深、沉积物特征、流量、流速和海平面等实地数据支持。本工作是基于使用Delft3D软件实现的米尼奥河河口数值模型。该模型能够模拟不同时间尺度的水动力和形态动力过程。使用OpenDA工具进行校准,该工具自动确定一些模型参数,如潮汐成分和粗糙度系数,旨在最大限度地减少观测数据与模拟结果之间的误差。根据政府间气候变化专门委员会(IPCC)第五次评估报告,考虑了不同的情景来评估气候变化的影响。结果表明,根据所考虑的情景,河口高度可达77 cm。洪水是河口泥沙输运的主要驱动因素,加剧了河口泥沙的吸积过程。此外,海平面上升减少了向海岸平台输送的沉积物量,增加了该地区的侵蚀风险,增加了河口内的增积。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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