THE EFFICACY OF INTERFEROMETRIC SONAR TO MAP THE SEAFLOOR IN VERY SHALLOW WATERS: CAPE COD NATIONAL SEASHORE AND VICINITY
The interferometric sonar system for this project collects coincident, high resolution imagery and bathymetry at 200 kHz. The unit is pole-mounted on to the bow of the research vessel. A real time kinematic Global Positioning System (GPS) is used for positioning and tide corrections. A dual antenna, differential GPS provides vessel heading and a motion reference unit gathers information primarily on vessel pitch and roll. A sound velocity probe collects data during surveys to increase the accuracy of the two-way travel time of sound through sea water.
Initial reconnaissance surveys conducted in the fall of 2009 in 1-5 m of water have been encouraging. Over 100 km of survey lines have been collected. Swath width to depth ratios have reached 10:1 in these shallow waters. Bedforms spaced at approximately 20-30 cm are readily discernible in the sidescan imagery. Uncertainty analyses are ongoing but initial results are similar to those attributed to this system for across track resolution: 4-5 cm in the sidescan imagery; and 5-6 cm in the bathymetry. Similar results are expected for the vertical resolution of the bathymetric data.
In the 2010 field season data will be collected to produce a seamless, tide-coincident, onshore-offshore map. Using terrestrial lidar the beach-dune system will be mapped at low tide followed by a vessel-based survey at high tide. The area to be mapped in Cape Cod Bay has a 3 m tidal range which will facilitate the spatial overlap of the lidar survey and the vessel-based survey throughout most of the study area.