Drifting buoys are generally attached to some form of drogue or sea-anchor, are easy to deploy, are relatively inexpensive to operate and reliably measure the atmosphere and ocean surface conditions, for an average of 18 months. Drifting buoys have a long history of use in oceanography, principally for the measurement of currents. There have also been many types of drifting buoys used for meteorological purposes since the First GARP Global Experiment (FGGE) in the 1970s.

The DBCP has been working for decades to design standardised drifting buoys to suit observational requirements for meteorological and oceanographic applications. Buoys that track surface currents in this way are called Lagrangian drifters and track ocean currents at the depth corresponding to the length of their drogue whilst collecting surface and subsurface measurements.

Lagrangian drifters were first designed and deployed in the world oceans in the context of the Surface Velocity Program (SVP) of the World Ocean Circulation Experiment (WOCE) and the Tropical Ocean and Global Atmosphere Program (TOGA), which became the Global Drifter Program (GDP). These SVP drifters were standardized in 1991, with small spherical hull and floats, and large Holey-Sock drogue centred at 15 meters below the surface. In 1993, drifters with barometer ports, called SVPB drifters, were tested in the high seas and proven reliable.

The Lagrangian Barometer Drifter, designed by the GDP, is now commercially available at low cost, and meets both oceanographic requirements (research: measurements of sea surface currents and sea temperature) and meteorological requirements (operational: sea surface temperature and air pressure). The DBCP has now mostly standardised on the use of SVP and SVP buoys, and their variants for the high seas.

Drifting buoys are generally attached to some form of drogue or sea-anchor, are easy to deploy, are relatively inexpensive to operate and reliably measure the atmosphere and ocean surface conditions, for an average of 18 months. Drifting buoys have a long history of use in oceanography, principally for the measurement of currents. There have also been many types of drifting buoys used for meteorological purposes since the First GARP Global Experiment (FGGE) in the 1970s.

Ice buoys have been used extensively in Arctic and Antarctic regions to track ice movement and are available commercially for deployment by ships or aircraft. Such buoys are equipped with low temperature electronics and lithium batteries that can operate at temperatures down to -50°C. In addition to the regularly-computed Argos locations the ice buoys can be equipped with satellite navigation receivers (e.g. GPS) which can compute even more accurate positions.

Are anchored at fixed locations and regularly collect observations from many different atmospheric and oceanographic sensors. Moored buoys are usually deployed to serve national forecasting needs, maritime safety needs or to observe regional climate patterns.

Moored buoys are normally relatively large and expensive platforms. They can vary from a few meters in height and breadth, to over 12 meters. Measurements from the mooring include surface variables (wind, air and sea surface temperature, salinity, air pressure), as well as subsurface temperatures down to a depth of 500 plus meters.

Data are usually collected through one of Argos, Iridium, ORBCOMM, GOES or METEOSAT, transmitted in real-time and shared on the GTS of WMO. They are generally upgraded or serviced yearly. They need to be constructed of very hardy materials to avoid problems in storms or high seas, the tether line which holds the buoy in the desired location needs to be especially strong. The design also needs to counter intentional vandalism or accidental damage. Many different designs exist for moored buoys depending on the ocean area.

As they are recording so many measurements, the moorings often store more data on-board than they send in real time, so when a moored buoy is recovered, processing and analysis of the data is performed at the buoy owner's data center.

If a moored buoy goes adrift it represents a potential loss of costly equipment and a possible hazard to navigation. For this reason a backup location system is used to ensure that an alert is sent if the buoy leaves a certain area.

A major part of the DBCP's moored buoy network is the Tropical Moored Buoy Implementation Panel array, which has arrays of moorings in each ocean basin and are used to monitor large scale phenomenon such as El Niño and the Southern Oscillation, showing the importance in the annual variability of global climate.

Most of the buoys in these arrays are the ATLAS mooring, developed at NOAA's Pacific Marine Environmental Laboratory (PMEL) Seattle, WA, in the 1980's, is a taut wire surface mooring with a tube-like float. It is deployed in depths of up to 6000 meters. Measurements from the mooring include surface variables, as well as subsurface temperatures down to a depth of 500 meters. This array and its planned expansion is the result of international collaboration between scientists from France, Japan, Korea, Indonesia, Western Africa, India and the USA.

Wave buoys are specialized ocean observing instruments designed to measure key characteristics of waves, including height, period, and direction. They are deployed in offshore, coastal, and large inland waters to monitor changing and sometimes hazardous sea conditions that can affect navigation, coastal erosion, and maritime safety. Equipped with sensors and wireless data transmission systems such as 4G LTE or Iridium satellite, wave buoys deliver near real-time information to data centers from virtually any location worldwide, supporting researchers, ship operators, offshore industries, and weather forecasters.

Modern meteorological and oceanographic forecasting systems rely on wave buoys to capture and analyze ocean surface dynamics. By recording the frequency and energy of waves—known as the wave spectrum—these buoys provide valuable parameters such as significant wave height, dominant wave period, and direction of wave propagation. This data enhances wave and swell prediction models, improving early warnings for dangerous sea states and contributing to the protection of lives, infrastructure, and coastlines.