Field Work Photo Gallery
Preparing the SonTek Hydra ADV for deployment.
Configuring the ADV software before deployment.
Ready for some marsh wading.
The deployed ADV, exposed during low tide.
Steven Traynum configures the ADV software before deployment. This ADV data was our basis of comparison when assessing the accuracy of current measurements recorded by a HF radar system deployed in the same area.
The CODAR RiverSonde HF radar stationed at the Baruch Institute as part of a study assessing the feasibility of using a HF radar system in an inter-tidal environment.

These are clod cards, shown after deployment. Clod cards are plaster of Paris blocks that dissolve at a fixed rate. By measuring the extent of of erosion during deployment, one can estimate the shear stress near the sea bed. Thus, clod cards are a relatively inexpensive method for measuring near-bottom flow patterns.

Climbing on board the submersible as part of the research cruise aboard the R.V. Seward Johnson. This cruise was studying physical and biological dynamics of the Charleston Bump, a large seafloor protrusion off the coast near Charleston, SC.
This study deployed two ADVs, shown here exposed at low tide, in order to determine the impact of bank roughness on flow. The left bank is a oyster bed (high roughness coefficient), whereas the right bank is a mud flat (very low roughness coefficient).
During the deployment period, we repeatedly ran boat wake trials. By driving a boat over the sensors during high tide, we generated a very strong flow in this system. We are interested in determining how the roughness of the tidal creek bank (oyster bed vs. mud flat) affects the dynamics of the flow.
Installing a WERA HF Radar system on Pritchard's Island, SC. This is a joint project between South Carolina and Georgia; a similar radar system is installed at St. Catherine's Island, GA. At each site, twelve receiver antennas are positioned along the beach, along with transmitter antennaes slighter further inland. The coverage zone spans Beaufort SC to Savannah GA and extends 150 miles (240 kilometers) offshore. This system will provide real-time surface current measurements every 15 minutes.
Now, read more about these projects and others HERE
  Boundary Layer Stress And Sediment Transport Laboratory
Department of Geological Sciences
Marine Science Program
University of South Carolina