首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Recent morphodynamic evolution of the largest uninhibited island in the Yangtze (Changjiang) estuary during 1998-2014: Influence of the anthropogenic interference
【24h】

Recent morphodynamic evolution of the largest uninhibited island in the Yangtze (Changjiang) estuary during 1998-2014: Influence of the anthropogenic interference

机译:1998-2014年期间长江(长江)河口最大的非抑制岛最近的形态动力学演化:人为干扰的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Estuarine geomorphology worldwide has greatly changed in the Anthropocene due to intensive human inferences in river basin and within estuary, which has received increasing global concerns. Here, recent morphodynamic evolution of Jiuduan Shoal (JDS), the largest uninhabited island in the Yangtze (Changjiang) Estuary, and associated controlling factors were analyzed based on unique high-resolution seasonal-surveyed bathymetric data during 1998-2014. It can be indicated that JDS presents novel 12 and 48 months fluctuations though significant accretion was detected on high flats above - 2 m. Meanwhile, morphodynamic evolution of JDS during 1998-2014 was divided into three stages: significant siltation on landward half of north JDS and expanding of Jiangya Shoal (JYS, part of JDS) tail, but less accretion at high flats from 1998 to 2002; continuous variations of JYS and reshape of seaward JDS with erosion band and heave appearance from 2002 to 2006; retentive alteration of JYS but recovery of erosion band and heave, together with redistribution of sand between high and low flats on seaward JDS after 2007. Moreover, river discharge could be likely the key factor controlling periodic characteristics of recent JDS evolution. Deep waterway project (DWP) dominates area increase of JDS by inducing accretion in north edge and south edge of Lower Shoal between 1998 and 2014. (C) 2016 Elsevier Ltd. All rights reserved.
机译:由于人类对流域和河口的深入推断,人类世间的全球河口地貌发生了很大变化,这引起了全球越来越多的关注。在这里,基于独特的高分辨率季节调查的测深数据,分析了长江(长江)河口最大的无人岛九段浅滩(JDS)最近的形态动力学演变以及相关的控制因素。可以表明,尽管在2 m以上的高单位上发现了明显的积聚,但JDS出现了12和48个月的新颖波动。同时,1998-2014年JDS的地貌动力学演化分为三个阶段:1998年至2002年JDS北部向陆一半的显着淤积和江雅浅滩(JYS,JDS的一部分)尾部的扩展,但高平地上的积聚较少;从2002年到2006年JYS的连续变化和海蚀JDS的重塑具有侵蚀带和隆起外观; JYS的保持性改变,但侵蚀带和隆起的恢复,以及沙质在2007年之后在海上JDS的高低平地之间的重新分布。此外,河流流量可能是控制近期JDS演变的周期性特征的关键因素。在1998年至2014年之间,深水航道项目(DWP)通过在下浅滩的北边缘和南边缘引起增生来主导JDS的面积增加。(C)2016 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
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