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Spit and Inlet Morphodynamics of a Tropical Coastal Lagoon

机译:热带沿海泻湖的吐水和入口形态动力学

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摘要

The morphological changes of spits and inlets of the Chilika lagoon, the largest brackish water tropical coastal lagoon in Asia, are investigated using real-time kinematic GPS observation and numerical models during 2009-2013. The seasonal/interannual variations of the spit and inlet cross-sectional areas with varying widths and depths are recorded in association with different physical processes. The results show significant changes in spit morphology: particularly, the south spit accreted continuously, while the middle and north spits eroded. The cross-sectional depth of inlets becomes narrower and deeper during summer and winter seasons, while they are wider and shallower during the monsoon. The model results show that sediment transport rate is larger during monsoon and summer, while it is relatively less during the winter. Alongshore, sediment transport is predominantly northward throughout the study period. The result shows that gain/loss of the spits and closure/opening of inlets are significantly controlled by the high wave power, longshore drifts, and river discharge. The study demonstrates that the combined use of observational and numerical models is very effective to understand the changes of spit and inlet morphology and their impact on ecological conditions of the lagoon environment.
机译:利用实时运动GPS观测和数值模型,研究了亚洲最大的半咸水热带沿海泻湖Chilika泻湖的出水口和入口的形态变化。与不同的物理过程相关联地记录了随宽度和深度的变化而变化的唾液和入口横截面的季节性/年际变化。结果表明,唾液形态发生了显着变化:特别是,南部的唾液不断分泌,而中部和北部的唾液逐渐腐蚀。在夏季和冬季,入口的横截面深度变得越来越窄,而在季风期间则变得越来越宽。模型结果表明,在季风和夏季,泥沙输送速率较大,而在冬季则相对较小。在整个研究期内,沿岸沉积物主要是向北迁移。结果表明,高波功率,长岸漂流和河水排放量极大地控制了污水口的损益和进水口的关闭/打开。研究表明,观察模型和数值模型的组合使用对于了解唾液和入口的形态变化及其对泻湖环境生态条件的影响非常有效。

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