Abstract:
Tidal asymmetry is a key factor in the geomorphology of many coastal lagoons. Whilst tidal asymmetry in
semi-diurnal tidal regimes has been extensively studied, its occurrence in mixed tidal regimes is less well
understood, and has a number of unique causes and characteristics. Tidal phase duration analysis and
least squares harmonic analysis have been used to study the temporal and spatial nature of asymmetry
in both offshore and coastal lagoon tides at the Murray Mouth in south-eastern Australia. GIS analysis of
bathymetric survey data has been used to study the roles of lagoon bathymetry on tidal distortion.
Tidal asymmetry in the Murray Mouth coastal lagoon results from frequency relationships between major
astronomical driving tides as well as bathymetry-induced tidal transformations. The frequency difference
between the K1 and S2 tides produces an important 6-monthly ebb/flood-dominant asymmetry cycle in the
incoming oceanic tides, whilst phase relationships between the K1 and K2 tides contribute to persistent
asymmetry. The use of standard relationships between theM2 andM4 tides as asymmetry indicators is shown to
be invalid for this mixed tidal regime. In this shallow, microtidal system, the impacts of bathymetry on tidal
asymmetry within the lagoon are profound, with inlet and channel configurations identified as the most
important controlling factors.
The results of this study may inform the strategic management of tidal inlets in mixed tidal regimes, such
as the Murray Mouth, that are subject to intermittent or long-term constriction.