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Numerical Analysis of the Influence of Sea Level Rise on Flood and Tidal Stage in the Yangtze River Estuary

机译:海平面上升对长江口洪水阶段的影响数值分析

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A two-dimensional numerical model was set up to simulate the tidal current of the Yangtze River Estuary with MIKE21 FM. This model has been calibrated and validated with the observed tidal level. We simulated the change of flood and tidal stage in the Yangtze River Estuary after the sea level rising by 20~60cm. The simulate results indicate that: (1)With sea level rising, the extent of rise of the high tide is greater than that of rise of low tide. Under the same sea level rise, the closer to the lower reaches of the Yangtze River Estuary, the more obvious the increase in the low tide level is, the rise of the high tide does not change significantly. (2)For the changes of the tidal range increase, under the same sea level rise, the closer to the upper reaches of the Yangtze Estuary, the greater the tidal range increase is.
机译:设立了二维数值模型,以模拟长江口与Mike21 FM的潮流。该模型已经校准并验证了观察到的潮汐层。我们模拟了长江口洪水和潮汐阶段的变化,海拔20〜60厘米。模拟结果表明:(1)随着海平面上升,高潮的上升程度大于低潮升高的程度。在相同的海平面上升,越来越近于长江口的下游,越明显的涨潮水平越高,高潮的升高不会显着变化。 (2)对于潮汐范围的变化增加,在相同的海平面上升,长江河口的上游越近,潮汐范围越大。

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