...
首页> 外文期刊>Journal of Hydrology >Changes in the physical characteristics of the water column at the mouth of a torrent during an extreme rainfall event
【24h】

Changes in the physical characteristics of the water column at the mouth of a torrent during an extreme rainfall event

机译:极端降雨事件中洪流口水柱物理特性的变化

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

The city of Genoa (Italy) was hit by a severe flash flood on the 4th November, 2011. The effects of this event on the water column at the mouth of the Polcevera Torrent, the main water course flowing into the Port of Genoa, are presented in this paper. The hydrological characteristics were measured with two conductivity-temperature-depth probes equipped with a turbidimeter, one fixed on the port breakwater and one used at mobile stations around the mouth of the torrent. The dynamics were measured with a horizontal acoustic Doppler current profiler (H-ADCP) fixed on the breakwater. Data collected before, during and after the flash flood were analysed to quantify the changes due to the event. The weather conditions during the event showed extremely heavy rain associated with strong weather instability, the convergence of a low-level southerly flow and the persistence of a squall line over a restricted area. The temperature, salinity, turbidity and dissolved oxygen measurements taken during the event showed the strong influence of the weather conditions and the fresh water input of the torrent itself on the water column at its mouth, an influence that dissipated during the following days. Instead, the dynamics measured at the mouth of the torrent were affected more by the strong south-easterly wind and the sea than the flow of fresh water. (C) 2015 Elsevier B.V. All rights reserved.
机译:热那亚市(意大利)在2011年11月4日遭受了严重的山洪袭击。该事件对流入热那亚港的主要水道Polcevera Torrent口的水柱的影响是在本文中提出。水文特征是用两台装有浊度计的电导率-温度-深度探头测量的,其中一根固定在防波堤上,另一根用于洪流口周围的移动台。用固定在防波堤上的水平声多普勒电流剖面仪(H-ADCP)测量动力学。分析在山洪暴发之前,之中和之后收集的数据,以量化该事件引起的变化。事件期间的天气状况显示,下雨特别严重,与强烈的天气不稳定,低水平的南风汇流和a线在限制区域上的持续存在有关。事件期间进行的温度,盐度,浊度和溶解氧测量结果显示,天气条件和山洪本身的淡水输入对其口处的水柱有很大的影响,此影响在随后的几天中逐渐消失。取而代之的是,在山洪口处测得的动力学受到的强烈东南风和海洋的影响大于淡水的流动。 (C)2015 Elsevier B.V.保留所有权利。

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