On the vertical structure of the Rhine region of freshwater influence

Abstract

An idealised three-dimensional numerical model of the Rhine region of fresh water influence (ROFI) was set up to explore the effect of stratification on the vertical structure of the tidal currents. Prandle's dynamic Ekman layer model, in the case of zero-depth-averaged, crossshore velocities, was first used to validate the response of the numerical model in the case of barotropic tidal flow. Prandle's model predicted rectilinear tidal currents with an ellipse veering of up to 2%. The behaviour of the Rhine ROFI in response to both a neap and a spring tide was then investigated. For the given numerical specifications, the Rhine plume region was well mixed over the vertical on spring tide and stratified on neap tide. During spring conditions, rectilinear tidal surface currents were found along the Dutch coast. In contrast, during neap conditions, significant cross-shore currents and tidal straining were observed. Prandle's model predicted ellipse veering of 50%, and was found to be a good indicator of ellipticity magnitude as a function of bulk vertical eddy viscosity. The modelled tidal ellipses showed that surface currents rotated anti-cyclonically whereas bottom currents rotated cyclonically. This caused a semi-diurnal cross-shore velocity shearing which was 90°out of phase with the alongshore currents. This cross-shore shear subsequently acted on the horizontal density gradient in the plume, thereby causing a semi-diurnal stratification pattern, with maximum stratification around high water. The same behaviour was exhibited in simulations of a complete spring-neap tidal cycle. This showed a pattern of recurring stratification on neaps and de-stratification on springs, in accordance with observations collected from field campaigns in the 1990's. To understand the increase in ellipticities to 30% during neaps and the precise shape of the vertical ellipse structure, stratification has to be taken into account. Here, a full threedimensional numerical model was employed, and was found to represent the effect of de-coupling of the upper and lower layers due to a reduction of mixing at the pycnocline.

Simultaneous measurements of tidal straining and advection at two parallel transects far downstream in the Rhine ROFI

“…Previous studies indicated a stratified state only during neap tides (periods of low energy) and a mixed state during spring tide (Simpson et al 1990;de Boer et al 2006). Here, we find that 1 day before spring tide stratification still occurs.…”

Numerical investigations of the turbulent kinetic energy dissipation rate in the Rhine region of freshwater influence

“…The Rhine ROFI is simulated by means of the grid de Boer et al (2006) used for their investigations. It is a rectilinear grid with grid cells of 500 m × 500 m close to the plume region and zooming out toward the northwest (left) and -east (top) boundary (see Fig.…”

Field Observations of Tidal Flow Separation at a Mega-Scale Beach Nourishment

“…Approximately 10 km South of the meganourishment, the fresh water runoff of the river Rhine is discharged into the North Sea, see Figure 2. This adds significant density differences to the system (De Boer, 2009). In the vicinity of the river mouth, fresh water is discharged in a pulsating fashion, with large outflow during low water (LW) and limited outflow during high water (HW).…”