Weather buoy tropical Pacific Ocean helped study the El Niño-Southern Oscillation. Moored weather buoys range from in diameter, while drifting buoys are smaller, with diameters of . Drifting buoys are the dominant form of weather buoy in sheer number, with 1250 located worldwide. Wind data from buoys has smaller error than that from ships. There are differences in the values of sea surface temperature measurements between the two platforms as well, relating to the depth of the measurement and whether or not the water is heated by the ship which measures the quantity. The first known proposal for surface weather observations at
Ocean observations of oceanic observation systems: Ocean observations The following are considered essential ocean climate variables by the Ocean Observations Panel for Climate (OOPC) that are currently feasible with current observational systems . Air Temperature Precipitation (meteorology) evaporation Air Pressure, sea level pressure (SLP) Surface radiative fluxes Surface thermodynamic fluxes Wind speed and direction Surface wind stress Water vapor Sea surface temperature (SST) Sea surface salinity (SSS) Sea level Sea state Sea ice Ocean current Ocean color (for biological activity) Carbon dioxide partial pressure (pCO2) There is a composite network of satellites that generate observations. These include: There is a composite network