Vignettes > Tidal Currents in a Microtidal Estuary - Port Stephens, Australia

Tidal Currents in a Microtidal Estuary - Port Stephens, Australia

Timothy Austin
School of Geosciences, University of Sydney
Author Profile

Shortcut URL: http://serc.carleton.edu/36119

Location

Continent: Australia
Country: Australia
State/Province:New South Wales
City/Town: Port Stephens
UTM coordinates and datum: none

Setting

Climate Setting: Humid
Tectonic setting:
Type: Process


Aerial photography showing the entire Port Stephens estuary and its location in Australia (top left water mark). Details


Photograph showing the erosion that is threatening property and infrastructure at Jimmy's Beach on the northern shoreline of Port Stephens. Details


Plot showing the residual mean current velocities and mean current durations. Positive residuals indicate flood phase and negative residuals indicate ebb phase. Red dashed vertical lines indicate deployments were recorded over a different time period. Details


Aerial photograph showing the deployment locations and combined current velocity and duration index with dominant flow direction. Arrows are drawn to scale relative to index such that a longer arrow indicates a greater velocity or duration asymmetry. Details



Description

Port Stephens is a popular tourist destination located on the mid-north New South Wales (NSW) coast, 230 km north of Sydney, Australia (Figure 1). Despite the regions popularity, it is not protected from the forces of nature and the wide-spread problem of coastal erosion that threatens the recreational value and infrastructure of the area (Figure 2). To successfully manage coastal erosion it is necessary to understand the processes responsible for the erosion, transportation and deposition of sediment.

Port Stephens is an estuary, which is a term used to describe an area that is the interaction of freshwater and marine systems. In this particular setting the freshwater or fluvial influences are largely confined to the western basin and the marine influences dominate the eastern basin (Figure 1). Marine influences refer to the supply of sediment to the estuary and the processes (waves and tidal currents) which are responsible for eroding, transporting and depositing this sediment.

A study is being undertaken to better understand these processes. The first step of this process is to record the tidal currents at representative locations throughout the eastern basin. This is achieved using two Acoustic Döppler Current Profilers (ADCP). These instruments are mounted on the sea floor and are capable of simultaneously recording the water velocity and direction at different depths above the instrument. This has been done at nine locations over a period of 13 months (Nov. 2007 to Dec. 2008). This data can then be used to characterise tidal flow patterns and infer sediment transport pathways.

To characterise the tidal flow, the current velocity data has been depth-averaged and separated based on its flow direction. Currents flowing into the estuary (in this case, flowing to the west) are associated with a rise in the water level in the estuary and are referred to as 'flood' phase. Currents flowing out of the estuary (flowing to the east) and associated with a lowering of the water level in the estuary are referred to as 'ebb' phase.

If we assume the amount of sediment transported by moving water is proportional to the cube of the water velocity, then it can be inferred that the tidal phase with the greatest mean velocity will transport a greater amount of sediment (Fitzgerald and Nummedal, 1983). The current velocities associated with each tidal phase were averaged over the duration of the instrument deployments. The mean flood current velocity was then subtracted from the mean ebb current velocity to give a residual current velocity (Figure 3). This residual indicates the phase (current direction) that has the greater mean current velocity and is also referred as the dominant phase.

Finer sediments exhibit a lag between the flow velocity dropping below that needed to transport the sediment and the sediment being deposited. Thus, the duration that a current flows in a particular direction is also of significance when inferring sediment transport. The duration of each flow phase have been processed in the same way as the current velocity to produce a residual phase duration. Since both current velocity and duration play a role in the transport of sediment, the residuals of these two variables were combined to produce an index value. This index value represents the residual direction and magnitude of the tidal current flow. This can be visualised (Figure 4) and used to infer net sediment transport patterns prior to more detailed analysis.

Some interesting results were observed from this study, most notably the occurrence of 'double dominance', whereby a greater mean velocity in a particular direction (phase) is paired with longer flow durations in the same direction (phase) (Figure 3). There is a prevalence of flood dominated flows over the shallower regions of the basin and ebb dominated flows at the entrance. These results indicate a complex interaction between the tidal circulation patterns and the estuarine morphology evident in the large sand shoals or 'flood-tide delta' that can be seen in the eastern region of the aerial photograph (Figure 4).

Whilst these observations are preliminary, they are contributing to improving the understanding of the processes that drive changes in the morphology of estuaries. The morphology of the eastern estuary affects the processes that are responsible for the coastal erosion that is evident in Figure 2. This research is contributing to the understanding of the relationship between the processes and morphology of estuaries and how these affect the processes and morphology of related estuarine beaches. This understanding will better facilitate the successful management of these systems.

Associated References


« Effects of 4-Wheel Drive Vehicles on Beach Sediment Transport       Linear dune formation: Longitudinal elongation or local wind rifting? An example from the Strzelecki Desert, central Australia »