首页> 外文期刊>Earth Surface Dynamics Discussions >Analysis of the drainage density of experimental and modelled tidal networks
【24h】

Analysis of the drainage density of experimental and modelled tidal networks

机译:实验和模拟潮汐网络的排水密度分析

获取原文
           

摘要

Based on controlled laboratory experiments, we numerically simulate the initiation and long-term evolution of back-barrier tidal networks in micro-tidal and meso-tidal conditions. The simulated pattern formation is comparable to the morphological growth observed in the laboratory, which is characterised by relatively rapid initiation and slower adjustment towards an equilibrium state. The simulated velocity field is in agreement with natural reference systems such as the micro-tidal Venice Lagoon and the meso-tidal Wadden Sea. Special attention is given to the concept of drainage density, which is measured on the basis of the exceedance probability distribution of the unchannelled flow lengths. Model results indicate that the exceedance probability distribution is characterised by an approximately exponential trend, similar to the results of laboratory experiments and observations in natural systems. The drainage density increases greatly during the initial phase of tidal network development, while it slows down when the system approaches equilibrium. Due to the larger tidal prism, the tidal basin has a larger drainage density for the meso-tidal condition (after the same amount of time) than the micro-tidal case. In both micro-tidal and meso-tidal simulations, it is found that there is an initial rapid increase of the tidal prism which soon reaches a relatively steady value (after approximately 40 yr), while the drainage density adjusts more slowly. In agreement with the laboratory experiments, the initial bottom perturbations play an important role in determining the morphological development and hence the exceedance probability distribution of the unchannelled flow lengths. Overall, our study indicates an agreement of the geometric characteristics between the numerical and experimental tidal networks.
机译:在受控实验室实验的基础上,我们在小潮汐和中潮汐条件下,数值模拟了后垒潮汐网络的启动和长期演变。模拟的图案形成与实验室中观察到的形态学增长相当,其特征是起始速度相对较快,向平衡态的调整较慢。模拟的速度场与自然参考系统如微潮威尼斯泻湖和中潮瓦登海相吻合。特别注意排水密度的概念,它是根据未引导的水流长度的超标概率分布进行测量的。模型结果表明,超出概率分布的特征是近似指数趋势,类似于自然系统中的实验室实验和观察结果。在潮汐网络发展的初始阶段,排水密度大大增加,而当系统趋于平衡时,排水密度会降低。由于潮汐棱镜较大,因此潮汐盆地在中潮条件下(经过相同的时间)比小潮汐条件下的排水密度更大。在微潮汐和中潮汐模拟中,都发现潮汐棱镜最初迅速增加,很快就达到了一个相对稳定的值(大约40年后),而排水密度的调整则更加缓慢。与实验室实验相一致,初始底部扰动在确定形态发展以及因此确定未窜流长度的超标概率分布方面起着重要作用。总的来说,我们的研究表明数值和实验潮汐网络之间的几何特征是一致的。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号