NOAA’s Global Drifter Program is a globally collaborative research project that provides near real-time marine data for the world. It allows us to record data for weather forecasts, track decadal patterns, and pinpoint inter-annual climate variations like El Nino Southern Oscillation. Global drifters provide observational verification for weather models, calibrate satellite observations, and collect and transfer new data about the ocean temperature, currents and barometric pressure.
In a paper published in the Journal of Operational Oceanography, a team of scientists with the Physical Oceanography Division at AOML, the University of Santiago de Compostela in Spain, the University of Miami, the University of Hawaii, and the Commonwealth Scientific and Industrial Research Organisation (CSIRO) of Australia analyzed possible pathways to link the location of the found debris in the southwestern Indian Ocean with potential crash sites, probably in the eastern Indian Ocean.
If you’ve ever sailed aboard a ship in the coastal ocean, or checked a weather report before going to the beach, then you are one of many millions of people who benefit from ocean observations. NOAA collects ocean observations and weather data to provide mariners with accurate forecasts of seas, as well as coastal forecasts and even regional climate predictions. It takes a lot of effort to maintain observations in all of the ocean basins to support these forecasts, and NOAA certainly can’t do it alone. Partnerships are essential to maintaining a network of free-floating buoys, known as drifters, and NOAA’s latest partner is not your typical research or ocean transportation vessel: the six sailboats and crew currently racing around the world in the Volvo Ocean Race.
Drifting buoys are a primary tool used by the oceanographic community to measure ocean surface circulation at unprecedented resolution. A drifter is composed of a surface float, which includes a transmitter to relay data via satellite, and a thermometer that reads temperature a few centimeters below the air-sea interface. The surface float is tethered to a holey sock drogue (a.k.a. “sea anchor”), centered at 15 m depth. The drifter follows the ocean surface current flow integrated over the drogue depth.