Abstract

Many tidal influenced estuaries and coastal basins feature tidal amplification because of, e.g., convergence and reflection. Increasing amplification rates were observed in the Elbe estuary, with consequences for construction measures, nautical manoeuvring, flood protection, riverbed morphology and ecosystems. Although many studies were conducted investigating the tidal wave transformation in estuaries, studies based on spatially well-distributed empirical data covering periods over more than a year are rare. To fill this gap, a self-developed adapted harmonic analysis method of least squares was applied to hydrographs from 25 gauges, distributed over the tidal influenced estuary from the river mouth to the tidal border which is given by the weir 160 km upstream of the river mouth. The investigation period for the harmonic analyses covers a whole nodal cycle of 18.613 a beginning in the year 2000. The tidal constituents’ oscillatory behaviour including the appearance of compound tides, generated by nonlinear shallow water processes, and the formation of reflection induced partially standing waves are determined. The tidal constituents show shared frequency-group specific partial clapotis, but also have significant differences in amplification within those groups. The latter fact contributes to the detected inverse proportionality of tidal range amplification inside the estuary to incoming tidal wave height. As reflection can cause resonance in tidal influenced rivers, tests are developed to analyse whether criteria for resonance are met. To determine the system’s specific resonance frequency, a new method was introduced with the three-parameter Lorentzian curve-fitting. As the detected resonance frequency is not close to tidal frequencies, full-established resonance of the tidal wave and of the tidal constituents is not observed in the Elbe estuary. Migrating nodes of the partially standing tidal wave hint at increasing latent resonance.

Highlights

  • Introduction published maps and institutional affilVarious estuaries and coastal basins exhibit extreme tidal conditions compared to their adjoining open sea because of system internal tidal wave transformation

  • Tidal waves that fulfil the critical ratio of system length to tidal wavelength of approximately 1/4 further frequently increase tidal ranges

  • We present a detailed analysis of the tidal constituent specific oscillatory behaviour in an estuary, for the first time according to our findings, based on water level measurements covering the whole estuary in a high spatial resolution and a whole nodal cycle of

Read more

Summary

Introduction

Introduction published maps and institutional affilVarious estuaries and coastal basins exhibit extreme tidal conditions compared to their adjoining open sea because of system internal tidal wave transformation. Tidal waves that fulfil the critical ratio of system length to tidal wavelength of approximately 1/4 (quarter-wavelength criterion, which is known as resonance criterion) further frequently increase tidal ranges. In this case, the natural period of the oscillating system equals the exciter period of the tidal wave and resonance occurs [1]. An increasing number of tidal rivers and basins, e.g. Thames [5], Scheldt [6], Ems [7], Elbe [8], showed a critical evolution of tidal wave transformation, primarily associated with conducted river engineering measures.

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call