Scientists create bathymetric maps and products to illustrate the depth and shapes of underwater terrain, just as topographical maps represent three-dimensional features of above-sea terrain.
Knowledge of the seafloor’s shape is crucial for understanding ocean circulation patterns that influence ocean atmosphere processes, which distribute heat between the tropics and the poles —a key component of Earth’s climate system.
High-quality bathymetric maps are necessary for the designation of marine protected areas to conserve threatened ecosystems or habitats. And, detailed measurements of ocean depth are critical for predicting tsunami inundation.
In addition, ocean bathymetry is important for the study of tides, wave action, sediment transport, underwater geo-hazards, cable routing, fisheries management, resource exploration, and military and defense applications.
Despite decades of ocean mapping, there is still a gap in detailed bathymetric maps and products over large parts of the oceans.
To address this, the Nippon Foundation has partnered with the General Bathymetric Chart of Oceans (GEBCO) to launch the Seabed 2030 Project in 2017, and it is the only long-term international project with a mandate to map the entire ocean floor. Operating under the joint sponsorship of the International Hydrographic Organization (IHO) and the Intergovernmental Oceanographic Commission (IOC), Seabed 2030 takes responsibility for bringing collected depth data together, finding and highlighting the unmapped gaps, and coordinating efforts by working with the established ocean mapping community.
[This digital elevation model image for Barkley Sound on the west coast of Canada’s Vancouver Island shows the entrance to the Port Alberni Inlet.]
A handful of publicly available parameters of the marine environment were chosen based on discussions with the working group. In addition to bathymetric data coverage, the parameters listed below reflect the attributes a potential target area could possess to increase its suitability for future planned bathymetric surveys. Three categories of input parameters were identified:
[This map represents the three areas identified for high priority mapping in the North Atlantic Ocean. Courtesy of The Journal of Ocean Technology.]
The next step was to create a map that showed the suitability of every 400 x 400 km cell as a potential target site within the North Atlantic study area. The methodology involved a GIS-based overlay technique that included the parameters of the marine environment as individual layers and combined them to rank the suitability of a location as a target area for mapping. The results revealed the suitability of every area throughout the North Atlantic and highlighted three suggested pilot mapping sites. NOAA’s Office of Ocean Exploration and Research is now looking at these suggested areas as potential mapping sites for the 2018 and 2019 Okeanos Explorer field seasons.
Impressively, this algorithm can easily be adjusted to include new criteria and new data as they become available, providing an objective way to prioritize mapping areas, which can be adapted to other regions.
This new approach has the potential to take the mapping and ocean science community a step closer to filling the large mapping gaps in the North Atlantic and across the globe. Edited for WeatherNation by Meteorologist Mace Michaels