Morphological Dynamics on Tidal Inlet System by Generating Variability of Tidal-Wave Energy Regimes; A Process-Based Model Approach of Tide Dominated Case and Mixed Tide Dominated Case

H. Bachtiar, Habibur Rahman, Anggun Etika, Ni Luh Putu Adi Ariestuti, Leo Eliasta, A. Dastgheib, M. Wegen
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Abstract

A process-based approach of 2D morphodynamic modeling is an alternative technique to investigate the morphological evolution in the long-term period. In the conceptual model application, there is two methodologies of morphodynamic model; realistic-based model (short time scale model in days/months) and realistic-analogue model which is called process-based model (long time scale model in ~100 years). Realistic-based model is the representative of generating force with complexity of real condition model in the field, however process-based model is the simplification of forcing model by representing the major factor. In this study, the domain model is as the adaptation of Dutch Wadden Zee tidal inlet system. A couple model technique of Flow module (Delft3d) and Wave module (X-Beach) is implemented into the model system. The tidal forcing is based on one main harmonic tidal component of M2 and super harmonic tidal component of M4 and M6 from the analysis harmonic of ZUNO model. The wave forcing is 1.4 m and 330 deg as the representative wave climate condition in Wadden Zee. A process-based model shows that initially the morphological response leading into establish-state condition. Tidal wave propagation which leads to stronger cross-shore ebb-flow perpendicular to the coastline contributes in morphological evolution inside the basin and forming the outer part of the inlet (ebb-tidal delta). Wave induce current in mixed-tide energy case are as the major contribution of stirring up sediments from the sea bed, leads to transport sediment because of longshore currents process, undertow, mass transport.
潮汐进水口系统的形态动力学研究基于过程的潮汐主导案例和混合潮汐主导案例模型方法
基于过程的二维形态动力学建模方法是研究长期形态演化的一种替代技术。在概念模型的应用中,形态动力学模型有两种方法;基于现实的模型(以天/月为单位的短时间尺度模型)和基于过程的现实模拟模型(以~100年为单位的长时间尺度模型)。基于现实的模型是现场真实条件模型中产生复杂力的代表,而基于过程的模型是通过表示主要因素对力模型进行简化。本研究采用荷兰瓦登海入潮系统的域模型。在模型系统中实现了Flow模块(Delft3d)和Wave模块(X-Beach)的耦合建模技术。根据ZUNO模型的谐波分析,M2的一个主调和潮汐分量和M4和M6的超调和潮汐分量是潮汐强迫的基础。波浪强迫为1.4 m和330°,是瓦登海的代表性波浪气候条件。一个基于过程的模型表明,最初的形态响应导致建立状态条件。潮汐波的传播导致了更强的垂直于海岸线的跨岸退流,促进了盆地内部的形态演变,形成了入口的外部(退潮三角洲)。混合潮汐能情况下的波致流是搅动海床沉积物的主要贡献,由于岸流过程、底流、物质输运导致沉积物输运。
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