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Assessing hydrological effects of human interventions on coastal systems: Numerical applications to the Venice Lagoon

机译:评估人为干预对沿海系统的水文影响:威尼斯泻湖的数值应用

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The hydrological consequences of historical, contemporary and future human activities on a coastal system were investigated by means of numerical models. The changes in the morphology of the Lagoon of Venice during the last century result from the sedimentological response to the combined effects of human interventions on the environment and global changes. This study focuses on changes from 1927 to 2012 and includes the changes planned for the protection of the city of Venice from storm surges and exceptional tides under future sea level rise scenarios. The application of a hydrodynamic model allowed for the analysis of the morphological effects on the lagoon circulation, the interaction with the sea and the internal mixing processes. The absolute values of the exchange between the lagoon and sea increased from 1927 to 2002 (from 3900 to 4600 m3 s-1), while the daily fraction of lagoon water volume exchanged decreased. At the same time, the flattening of the lagoon and loss of morphological heterogeneity enhanced the internal mixing processes driven by the tide and wind, reducing thus the overall water renewal time from 11.9 days in 1927 to 10.8 days in 2002. Morphological changes during the last decade reduced the water exchange through the inlets and induced an increase of the basin-wide water renewal time of 0.5 day. In the future, Venice Lagoon will evolve to a more restricted environment due to sea level rise, which increases the lagoon volume, and periodical closure of the lagoon from the sea during flooding events, which reduces the communication with the open sea. Therefore, the flushing capacity of the lagoon will decrease considerably, especially in its central part. Furthermore, some considerations on the impact of the hydromorphological changes on the ecological dynamics are proposed.
机译:通过数值模型研究了历史,当代和未来人类活动对沿海系统的水文后果。上个世纪威尼斯泻湖形态的变化是由于人类活动对环境和全球变化的综合影响所产生的沉积学响应所致。这项研究的重点是从1927年到2012年的变化,其中包括计划在未来海平面上升的情况下保护威尼斯市免受风暴潮和特殊潮汐影响的变化。水动力模型的应用允许分析对泻湖环流,与海洋的相互作用以及内部混合过程的形态学影响。泻湖与海洋之间交换的绝对值从1927年到2002年(从3900立方米到4600立方米s-1)增加,而每天交换的泻湖水量的比例却减少了。同时,泻湖的平坦化和形态异质性的丧失增强了由潮汐和风驱动的内部混合过程,从而使总的换水时间从1927年的11.9天减少到2002年的10.8天。最后一次的形态变化十年减少了通过进水口的水交换,并导致整个流域的换水时间增加了0.5天。将来,威尼斯泻湖将因海平面上升而演变为更加受限制的环境,这将增加泻湖的体积,并在洪灾期间定期将泻湖与海隔离,从而减少与公海的通讯。因此,泻湖的冲洗能力将大大降低,特别是在其中心部分。此外,提出了对水形态变化对生态动力学影响的一些考虑。

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