A stainless steel instrument frame was constructed at NPS to mount oceanographic instruments about 1m above the sandy bed. The frame and instruments were assembled at the marine operations building at NPS, then trucked up to the "John Martin" research vessel at Moss Landing Marine Labs and loaded on to the boat by crane. When the boat was at the selected site in 12m depth, offshore from the marine operations building, the frame was lowered to the bed and "jetted" into the sandy bed using water jets guided by divers. The following day the multi fiber and conductor cable was pulled offshore from the Marine operations building and connected to the instrument central electronics package by divers. The rugged instrument frame and high bandwidth communications and power cable allow long term observations of inner shelf processes using sophisticated instrument systems.
The instruments on the frame and their function are listed below:
A high precision digital pressure sensor measures the height of water above the frame, to produce a record of tides and long period waves. The power spectrum of the surface waves can be calculated from these pressure timeseries.
An Acoustic Doppler Current Profiler (ADCP) measures the water current every 1m (39") from the frame to the near ocean surface. This allows the mean currents and wave signatures of surface waves to be determined.
A high resolution Bistatic Coherent Doppler Velocity and Sediment Profiler (BCDVSP) developed at NPS by the ocean turbulence research group measures the complete velocity vector and sediment concentration every 1cm over a 60 cm range above the bed. These small scale measurements are used to define the mean and turbulent structure of the water column above the sandy bed which results from mean currents and wave induced curents interacting with the bed.
A scanning Acoustic Altimeter (SAA) developed by the ocean turbulence research group continuously maps the sandy bed below the BCDVSP. It is now set up to scan a 2m by 2m area wth .5cm vertical and 2cm horizontal resolution, allowing the changing bumps and ripples on the bed to be measured even in optically opaque, turbid water conditions. A Structured Light And Camera (SLAC) developed by the ocean turbulence research group continuously images a 1m by 1m area under the BCDVSP. The small scale bed forms can be quantified using thin sheets of light which illuminate parts of the sandy bed.