WAIMOS is a science node of the IMOS in Western Australia where the main area of interest is the continental shelf and slope regions offshore Rottnest. Within this region there are important topographic features such as the Rottnest Island and Perth Canyon and the circulation is dominated by the southward flowing Leeuwin Current (LC) with the northward flowing wind driven Capes Current (CC). The IMOS infrastructure located in this region includes HF Radar (CODAR and WERA systems) for surface currents; Ocean gliders (Slocum) for subsurface water properties; continental shelf moorings (ADCP, thermistor); and, remotely sensed data products (SST and ocean colour). This is the only observing system globally that has different platforms collecting sustained data for almost two decades. Example data collected from these instruments will be presented, an example of integration of different data sets. These include: (1) Interaction between the LC and CC. Here, the southward Leeuwin Current interacts with northward Capes Current to create both mesoscale and sub-mesoscale eddies; (2) dense water transport along the continental shelf a unique flow feature; (3) diurnal-inertial resonance that allows for wind mixing to extend to 500 m water depth.