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Assessment of sea-level rise impacts on salt-wedge intrusion in idealized and Neretva River Estuary

机译:评估海平面上升对理想化和内雷特瓦河河口盐楔入侵的影响

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Understanding the response of estuaries to sea-level rise is crucial in developing a suitable mitigation and climate change adaptation strategy. This study investigates the impacts of rising sea levels on salinity intrusion in salt-wedge estuaries. The sea-level rise impacts are assessed in idealized estuaries using simple expressions derived from a two-layer hydraulic theory, and in the Neretva River Estuary in Croatia using a two-layer time-dependent model. The assessment is based on three indicators - the salt-wedge intrusion length, the seawater volume, and the river inflows needed to restore the baseline intrusion. The potential SLR was found to increase all three considered indicators. Theoretical analysis in idealized estuaries suggests that shallower estuaries are more sensitive to SLR. Numerical results for the Neretva River Estuary showed that SLR may increase salt-wedge intrusion length, volume, and corrective river inflow. However, the results are highly non-linear because of the channel geometry, especially for lower river inflows. A theoretical assessment of channel bed slope impacts on limiting a potential intrusion is therefore additionally discussed. This findings emphasize the need to use several different indicators when assessing SLR impacts.
机译:了解河口对海平面上升的反应对于制定合适的缓解措施和适应气候变化战略至关重要。这项研究调查了海平面上升对盐楔河口盐度入侵的影响。在理想河口中,使用源自两层水力理论的简单表达式来评估海平面上升的影响,而在克罗地亚的涅雷特瓦河河口中,则使用两层时变模型来评估海平面上升的影响。该评估基于三个指标-盐楔侵入长度,海水量和恢复基线侵入所需的河流流入量。发现潜在的SLR会增加所有三个已考虑的指标。理想河口的理论分析表明,较浅的河口对SLR更为敏感。 Neretva河口的数值结果表明,SLR可能会增加盐楔的侵入长度,体积和校正河流量。但是,由于河道的几何形状,结果是高度非线性的,特别是对于较低的河流入流。因此,还讨论了对通道床坡度对限制潜在侵入的影响的理论评估。这一发现强调了在评估SLR影响时需要使用几种不同的指标。

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