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A coupled analytical model for salt intrusion and tides in convergent estuaries

机译:收敛河口盐分和潮汐耦合分析模型

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In this paper we develop a coupled analytical model for salinity and tidal propagation in estuaries where the cross-sectional area varies exponentially. A simple analytical model for tidal dynamics has been used to estimate the tidal excursion, which has an important influence on the salt intrusion process since it determines the extreme salinities (i.e. salinity distribution for high water slack and low water slack). The objective of the coupling is to reduce the number of calibration parameters, which subsequently strengthens the reliability of the salt intrusion model. Moreover, the coupling enables us to assess the potential impacts of external changes, both human-induced interventions (e.g. dredging) and natural changes (e.g. global sea level rise), on the salt intrusion process. In addition, the fully analytical solution for hydrodynamics allows immediate estimation of the tidally averaged depth and friction coefficient for given water level recordings and salinity measurements. This is particularly useful when a geometric survey is not available. The coupled model has been applied to six previously unsurveyed estuaries in Malaysia and the results show that the correspondence between analytical estimations and observations is very good. Thus, the coupled model proves to be a useful tool to obtain estimates of salt intrusion in estuaries based on a minimum amount of information required and for assessing the effect of human-induced or natural changes.
机译:在本文中,我们开发了盐度和潮汐传播在河口横截面积成指数变化的耦合分析模型。一个简单的潮汐动力学分析模型已被用来估算潮汐偏移,这对盐分侵入过程有重要影响,因为它决定了极端盐度(即高水松弛度和低水松弛度的盐度分布)。耦合的目的是减少校准参数的数量,从而增强盐侵入模型的可靠性。此外,这种耦合使我们能够评估外部变化的潜在影响,包括人为干预(例如疏ed)和自然变化(例如全球海平面上升)对盐分入侵过程的影响。此外,针对流体动力学的完全分析解决方案可立即估算给定水位记录和盐度测量值的潮汐平均深度和摩擦系数。当没有几何测量时,这特别有用。耦合模型已被应用到马来西亚六个先前未调查的河口,结果表明分析估计和观测值之间的对应关系非常好。因此,事实证明,耦合模型是一种有用的工具,它可以基于所需的最少信息量来获得对河口盐分入侵的估计,并用于评估人为或自然变化的影响。

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