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Impact of sea level rise on tidal range in Chesapeake and Delaware Bays

机译:切萨皮克和特拉华湾海平面上升对潮汐范围的影响

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摘要

Coastal inundation is affected not only by rising mean sea level but also by changing tides. A numerical model is developed to investigate how sea level rise and coastline changes may impact tides in two coastal-plain estuaries, Chesapeake Bay and Delaware Bay. Despite their different tidal characteristics, the two estuaries display similar responses to the sea level rise and shoreline management scenarios. When hypothetic sea walls are erected at the present coastline to prevent low-lying land from flooding, tidal range increases, with greater amplification in the upper part of the two estuaries. When low-lying land is allowed to become permanently inundated by higher sea level, however, tidal range in both estuaries decreases. Analyses of the tidal energy budget show that the increased dissipation over the shallow water and newly inundated areas compensates for the reduced dissipation in deep water, leading to smaller tidal range. The changes in the tidal range are not proportional to the changes in the mean sea level, indicating a nonlinear tidal response to sea level rise. The ratio of tidal range change to sea level rise varies between −0.05 and 0.1 in Chesapeake Bay and between −0.2 and 0.25 in Delaware Bay. The model results suggest a potential adaptation strategy that uses inundation over low-lying areas to reduce tidal range at up-estuary locations.
机译:沿海淹没不仅受到平均海平面上升的影响,而且还受到潮汐变化的影响。建立了一个数值模型来研究海平面上升和海岸线变化如何影响切萨皮克湾和特拉华湾两个沿海平原河口的潮汐。尽管它们的潮汐特征不同,但两个河口对海平面上升和海岸线管理方案的反应相似。当在目前的海岸线上竖立假想的海堤以防止低洼土地泛滥时,潮汐范围将增加,两个河口的上部放大幅度更大。但是,当低洼的土地被更高的海平面永久性淹没时,两个河口的潮汐范围都会减小。潮汐能收支的分析表明,浅水区和新淹没区的耗散增加,弥补了深水区耗散的减少,导致潮汐范围变小。潮汐范围的变化与平均海平面的变化不成比例,表明潮汐对海平面上升的非线性响应。切萨皮克湾的潮汐变化与海平面上升的比率在-0.05和0.1之间以及在特拉华湾的-0.2和0.25之间变化。模型结果表明了一种潜在的适应策略,该策略利用低洼地区的洪水来减小河口上方的潮汐范围。

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