Add to ORKGWe consider the effects of coastal topography on the wake of an idealised headland model in a laboratory flume. Under a range of Reynolds numbers relevant to coastal oceans, we find that coherent eddies interact strongly with the headland shear layer and wake, affecting the width of the shear layer and the length of the wake. A preliminary investigation of turbulence statistics indicates that topography upstream of a headland can lead to a wider shear layer, a headland wake that extends further downstream, and enhanced horizontal diffusion out of the wake relative to the case with unperturbed oncoming flow
In the wakes of islands (or headlands), the presence of stratification higly modifies the structure ...
With increasing offshore wind development, more and more marine environments are confronted with the...
We investigate the formation and evolution of oceanic wakes, generated by obstacle of the shape of M...
We consider the effects of coastal topography on the wake of an idealised headland model in a labora...
The two-dimensional steady flow of a coastal flow past a headland has been considered. Results from ...
Large-eddy simulations are used to investigate the effects of coastal topography and atmospheric str...
This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical ...
Aerial photographs of transverse shear flows around islands in Rupert Bay, a shallow and turbid estu...
Observations of a front associated with boundary layer separation from a headland illustrate a mecha...
In this thesis, the phenomenon of flow-topography interaction is considered in the context of two dy...
A numerical study aimed at investigating the conditions under which different flow regimes appear ne...
This is a article on flow over topography named “Topographic eddies”. It covers the theory behind fl...
Because wind is one of the main forcings in storm surge, we present an idealised process-based model...
Little research was done in the past concerning the propagation of three dimensional effect in shall...
Atmospheric models are strongly dependent on the turbulent exchange of momentum, sensible heat and m...
In the wakes of islands (or headlands), the presence of stratification higly modifies the structure ...
With increasing offshore wind development, more and more marine environments are confronted with the...
We investigate the formation and evolution of oceanic wakes, generated by obstacle of the shape of M...
We consider the effects of coastal topography on the wake of an idealised headland model in a labora...
The two-dimensional steady flow of a coastal flow past a headland has been considered. Results from ...
Large-eddy simulations are used to investigate the effects of coastal topography and atmospheric str...
This is the publisher’s final pdf. The published article is copyrighted by the American Geophysical ...
Aerial photographs of transverse shear flows around islands in Rupert Bay, a shallow and turbid estu...
Observations of a front associated with boundary layer separation from a headland illustrate a mecha...
In this thesis, the phenomenon of flow-topography interaction is considered in the context of two dy...
A numerical study aimed at investigating the conditions under which different flow regimes appear ne...
This is a article on flow over topography named “Topographic eddies”. It covers the theory behind fl...
Because wind is one of the main forcings in storm surge, we present an idealised process-based model...
Little research was done in the past concerning the propagation of three dimensional effect in shall...
Atmospheric models are strongly dependent on the turbulent exchange of momentum, sensible heat and m...
In the wakes of islands (or headlands), the presence of stratification higly modifies the structure ...
With increasing offshore wind development, more and more marine environments are confronted with the...
We investigate the formation and evolution of oceanic wakes, generated by obstacle of the shape of M...