首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >River-tide dynamics: Exploration of nonstationary and nonlinear tidal behavior in the Yangtze River estuary
【24h】

River-tide dynamics: Exploration of nonstationary and nonlinear tidal behavior in the Yangtze River estuary

机译:潮汐动力学:长江口非平稳和非线性潮汐行为的探讨

获取原文
获取原文并翻译 | 示例
           

摘要

River-tide dynamics remain poorly understood, in part because conventional harmonic analysis (HA) does not cope effectively with nonstationary signals. To explore nonstationary behavior of river tides and the modulation effects of river discharge, this work analyzes tidal signals in the Yangtze River estuary using both HA in a nonstationary mode and continuous wavelet transforms (CWT). The Yangtze is an excellent natural laboratory to analyze river tides because of its high and variable flow, its length, and the fact that there are do dams or reflecting barriers within the tidal part of the system. Analysis of tidal frequencies by CWT and analysis of subtidal water level and tidal ranges reveal a broad range of subtidal variations over fortnightly, monthly, semiannual, and annual frequencies driven by subtidal variations in friction and by variable river discharges. We employ HA in a nonstationary mode (NSHA) by segregating data within defined flow ranges into separate analyses. NSHA quantifies the decay of the principal tides and the modulation of M_4 tide with increasing river discharges. M_4 amplitudes decrease far upriver (landward portion of the estuary) and conversely increase close to the ocean as river discharge increases. The fortnightly frequencies reach an amplitude maximum upriver of that for over tide frequencies, due to the longer wavelength of the fortnightly constituents. These methods and findings should be applicable to large tidal rivers globally and have broad implications regarding management of navigation channels and ecosystems in tidal rivers.
机译:人们对河潮动力学的了解仍然很少,部分原因是传统的谐波分析(HA)无法有效地应对非平稳信号。为了探索潮汐的非稳态行为和河流流量的调制效应,这项工作使用非稳态模式下的HA和连续小波变换(CWT)分析了长江口的潮汐信号。由于流量高,流量可变,长度长,而且在系统的潮汐部分内有水坝或反射屏障,因此长江是分析河流潮汐的出色天然实验室。通过CWT进行潮汐频率分析以及潮汐水位和潮汐范围分析显示,在两周,每月,半年和每年的频率下,潮汐变化范围很大,这是由潮汐摩擦力变化和河流流量变化驱动的。我们通过将定义的流量范围内的数据隔离到单独的分析中,以非平稳模式(NSHA)来使用HA。 NSHA量化了主要潮汐的衰减以及随着河水流量的增加对M_4潮汐的调制。随着河流流量的增加,M_4振幅减小到远处上游(河口的陆地部分),反之则增加到近海处。由于每两周成分的波长较长,所以每两周频率的振幅最大上升幅度超过潮汐频率。这些方法和发现应适用于全球范围内的大型潮汐河,并对潮汐河的航道和生态系统管理产生广泛的影响。

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